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["ObservationURI","ObservationName","WellType","HeaderURI","WellName","OtherID","County","State","LatDegree","LongDegree","LocationUncertaintyStatement","DepthTopInterval_ft","DepthBottomInterval_ft","RockType","Lithology","OtherLithologyName","GeologicUnitName","OtherFormationName","PercentTargetRock","AverageNetTargetRockThickness_m","AverageNetTargetRockThicknessUncertainty","AverageNetTargetRockThicknessMethodology","VerticalConductivity_ft_day","HorizontalConductivity_ft_day","SpecificStorage","UnitsStorage","Permeability","UnitsPermeability","PermeabilityMax","PermeabilityMin","PermeabilityAverage","PermeabilityAverageUncertainty","PermeabilityAverageMethod","SpecificYield_percent","Transmissivity","Transmissivity_units","EffectivePorosity","Porosity","PorosityMax_pct","PorosityMin_pct","PorosityAverage_pct","PorosityAverageUncertainty","PorosityAverageMethod","ObservationMethod","RelatedResource\n","Source","MetadataURI","Shape","CementationMineralogy","Trap","Drive","WaterDensity_mgL","CommodityOfInterest","Stimulation","AveragePerforatedThickness_m","WellCount","FaultCount","Faulted","FaultType","FaultHydraulicCharacter","FirstProductionDate","LastProductionDate","YearsInProduction","MonthlyProduction_bbl","ProductionReportDate","AverageMonthlyWaterProduction_bbl","MinimumMonthlyWaterProduction_bbl","MaximumMonthlyWaterProduction_bbl","WaterInjection_bbl","WaterSaturation_pct","WaterSaturationMethod","WaterSaturationUncertainty","WaterTDS_mgl","AverageInitialPressure_psi","AverageInitialPressure_Uncertainty","AverageInitialPressure_Methodology","AverageBHT_°F","BHT units","AverageBHT_Uncertainty","AverageBHT_Methodology","Maria reviewed","if statement (not visible)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Waskom Field",null,null,"Willow Springs Field","Willow Springs Field",null,"Woodlawn Field"]
[26,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",2058,null,"Sandstone",null,null,"Blossom Sandstone",null,null,{"$f":"17*0.3048","v":5.1816000000000004},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"struct-structural nose  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1963,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[8,null,null,null,null,"Willow Springs Field","Gregg","TX",32.521326640970337,-94.78636420539091,"Average of Field from DrillingInfo",8873,null,"Sandstone",null,null,"Bodenhem-Trans Sandstone",null,null,{"$f":"6*0.3048","v":1.8288000000000002},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct-facies change  strat-faulted anticline",null,null,"gas and oil",null,null,null,null,null,null,null,1966,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[48,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9653,9654,"Sandstone",null,null,"Cotton Valley Sandstone","Roseberry Interval",null,{"$f":" (M4-L4)*0.3048","v":0.30480000000000002},1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,2.1999999999999999E-2,"md",2.1999999999999999E-2,2.1999999999999999E-2,2.1999999999999999E-2,1,"Values from Bagley, 2009",null,null,null,null,2.2999999999999998,2.2999999999999998,2.2999999999999998,2.2999999999999998,1,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9653 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30570","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[47,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9619,9620,"Sandstone",null,null,"Cotton Valley Sandstone","Roseberry Interval",null,0.30480000000000002,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,2.5000000000000001E-2,"md",2.5000000000000001E-2,2.5000000000000001E-2,2.5000000000000001E-2,1,"Values from Bagley, 2009",null,null,null,null,7,7,7,7,1,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9619 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30569","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[47,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9565,9655,"Sandstone",null,null,"Cotton Valley Sandstone","Roseberry Interval",null,27.432000000000002,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,null,"md",0.3,0.01,{"$f":"(AC6+AD6)/2","v":0.155},5,"Values from Bagley, 2009",null,null,null,null,null,8,1,{"$f":"(AM6+AN6)/2","v":4.5},5,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9619 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30569","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[45,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9448,9449,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis I Interval",null,0.30480000000000002,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,5.5E-2,"md",5.5E-2,5.5E-2,5.5E-2,1,"Values from Bagley, 2009",null,null,null,null,5.3,5.3,5.3,5.3,1,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9448 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30566","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[45,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9450,9480,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis I Interval",null,9.1440000000000001,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,null,"md",0.1,0.01,{"$f":"(AC8+AD8)/2","v":5.5E-2},5,"Values from Bagley, 2009",null,null,null,null,null,7,1,{"$f":"(AM8+AN8)/2","v":4},5,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9448 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30566","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[44,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9431,9432,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis I Interval",null,0.30480000000000002,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,4.13,"md",4.13,4.13,4.13,1,"Values from Bagley, 2009",null,null,null,null,8.6,8.6,8.6,8.6,1,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9431 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30565","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[44,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9425,9435,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis I Interval",null,3.048,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,null,"md",6,1,{"$f":"(AC10+AD10)/2","v":3.5},5,"Values from Bagley, 2009",null,null,null,null,null,10,7,{"$f":"(AM10+AN10)/2","v":8.5},5,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9431 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30565","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[43,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9503,9504,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis II Interval",null,0.30480000000000002,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,6.4000000000000001E-2,"md",6.4000000000000001E-2,6.4000000000000001E-2,6.4000000000000001E-2,1,"Values from Bagley, 2009",null,null,null,null,4.5999999999999996,4.5999999999999996,4.5999999999999996,4.5999999999999996,1,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9503 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30568","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[43,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9508,9540,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis II Interval",null,9.7536000000000005,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,null,"md",0.15,1.4999999999999999E-2,{"$f":"(AC12+AD12)/2","v":8.249999999999999E-2},5,"Values from Bagley, 2009",null,null,null,null,null,12,4,{"$f":"(AM12+AN12)/2","v":8},5,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9503 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30568","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[42,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9511,9512,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis II Interval",null,0.30480000000000002,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,0.115,"md",0.115,0.115,0.115,1,"Values from Bagley, 2009",null,null,null,null,8.6999999999999993,8.6999999999999993,8.6999999999999993,8.6999999999999993,1,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9511 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30567","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[42,null,null,"\t4220330565",null,"Wildcatter","Harrison","TX",32.5787458,-94.260360599999998,"DrillingInfo",9490,9508,"Sandstone",null,null,"Cotton Valley Sandstone"," Davis II Interval",null,5.4864000000000006,1,"Calculated from top and bottom depths in Bagley, 2009",null,null,null,null,null,"md",0.15,0.01,{"$f":"(AC14+AD14)/2","v":0.08},5,"Values from Bagley, 2009",null,null,null,null,null,5,1.5,{"$f":"(AM14+AN14)/2","v":3.25},5,"Values from Bagley, 2009| Uncertainty 1=empirical related to formation 5=assigned from calc.","core plug @ 9511 ft","http://webapps.rrc.texas.gov/DP/publicQuerySearchAction.do?countyCode=203&apiSeqNo=30567","Bagley, 2009",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[33,null,null,null,null,"Henderson North Field","Rusk","TX",32.238958799999999,-94.802898740000003,"Average of Field from DrillingInfo",10400,10950,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"75*0.3048","v":22.86},1,"Average pay from Clawson, 1984",null,null,null,null,null,"md",0.1,0,0.05,5,"Mathematica  mean of values from Clawson, 1984",null,null,null,null,null,11,9,10,1,"Values from Clawson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Clawson, 1984",null,null,null,"stratigraphic","Gas dissolution",null,"oil and gas","acidized and fractured",null,null,null,null,null,null,"1979-11-26",null,null,null,null,null,null,null,null,"25-40",null,"Values from Clawson 1984",105700,5600,1,"IBHSIP Values from Clawson 1984",235,"Farhenheit",1,"Values from Clawson 1984","yes",{"$f":"IF(F15=$CC$1,AD15,\" \")","v":" "}]
[11,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",8400,9700,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"250*0.3048","v":76.2},1,"Average pay from Drake and Pendleton, 1984",null,null,null,null,null,"md",1,0,0.5,5,"Mathematical mean of values from Drake and Pendleton, 1984",null,null,null,null,null,8,8,8,1,"Values from Drake and Pendleton, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Drake and Pendleton, 1984",null,null,null,"structural-stratigraphic","Pressure Depletion",null,"oil and gas","acidized and fractured",null,null,null,null,null,null,"1970-04-08",null,null,null,null,null,null,null,null,35,null,"Values from Drake and Pendleton, 1984",124000,4800,1,"IBHSIP Values from Drake and Pendleton, 1984",240,"Farhenheit",1,"Values from Drake and Pendleton, 1984","yes",{"$f":"IF(F16=$CC$1,AD16,\" \")","v":" "}]
[46,null,null,null,null,"Oak Hill Field","Rusk","TX",32.331712323036847,-94.673940260897368,"Average of Field from DrillingInfo",9072,10454,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"(0.3048)*280","v":85.344000000000008},1,"Average pay from Farnham, 1984",null,null,null,null,null,"md",0.03,0.03,0.03,1,"Values from Farnham, 1984",null,null,null,null,null,10,10,10,1,"Values from Farnham, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Farnham, 1984",null,null,null,"structural-stratigraphic","Pressure Depletion",null,"oil and gas","Fractured",null,null,null,null,null,null,"1971-01-26",null,null,null,null,null,null,null,null,40,null,"Values from Farnham, 1984",220475,3296,1,"IBHSIP Values from Farnham, 1984",222,"Farhenheit",1,"Values from Farnham, 1984","yes",{"$f":"IF(F17=$CC$1,AD17,\" \")","v":" "}]
[27,null,null,null,null,"Hallsville South Field","Harrison","TX",32.394073473333336,-94.47491800666667,"Average of Field from DrillingInfo",9440,10583,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"260*0.3048","v":79.248000000000005},1,"Average pay from Farnham, 1984",null,null,null,null,null,"md",0.02,5.0000000000000001E-3,0.02,1,"Values from Farnham, 1984",null,null,null,null,null,9,9,9,1,"Values from Farnham, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Farnham, 1984",null,null,null,"structural-stratigraphic","Pressure Depletion",null,"oil and gas","Fractured",null,null,null,null,null,null,"1973-09-20",null,null,null,null,null,null,null,null,30,null,"Values from Farnham, 1984",230644,2435,1,"IBHSIP Values from Farnham, 1984",218,"Farhenheit",1,"Values from Farnham, 1984","yes",{"$f":"IF(F18=$CC$1,AD18,\" \")","v":" "}]
[82,null,null,null,null,"Oak Hill South Field","Rusk","TX",32.303937835714294,-94.644958264285705,"Average of Field from DrillingInfo",10070,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-structual nose  strat-faces change",null,null,"gas and oil",null,null,null,null,null,null,null,1979,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[78,null,null,null,null,"Woodlawn Field","Harrison","TX",32.647414041089128,-94.334453307095743,"Average of Field from DrillingInfo",9592,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"25*0.3048","v":7.62},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,"md",0.1,0.1,0.1,1,"Values from Kosters et al.,1989 (Table 37)",null,null,null,null,null,8,8,8,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"structural-stratographic (structural nose and facies change)",null,null,"oil and gas",null,null,null,null,null,null,null,1965,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,260,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 37)","yes"]
[58,null,null,null,null,"Waskom Field","Harrison","TX",32.469260472356183,-94.126346337569501,"Average of Field from DrillingInfo",8544,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"32*0.3048","v":9.7536000000000005},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,"md",0.09,0.09,0.09,1,"Values from Kosters et al.,1989 (Table 37)",null,null,null,null,null,12,12,12,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-anticline, dome  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1955,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,{"$f":"IF(F21=$CA$1,AD21,\" \")","v":" "},{"$f":"IF(F21=$CB$1,AD21,\" \")","v":" "},"yes"]
[52,null,null,null,null,"Blocker Field","Harrison","TX",32.448868573868339,-94.419515748148228,"Average of Field from DrillingInfo",9731,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"188*0.3048","v":57.302400000000006},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-structural nose  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1977,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[41,null,null,null,null,"Oak Hilll Field","Rusk","TX",32.331712323036847,-94.673940260897368,"Average of Field from DrillingInfo",10212,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"386*0.3048","v":117.6528},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,"md",0.03,0.03,0.03,1,"Values from Kosters et al.,1989 (Table 37)",null,null,null,null,null,9,9,9,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-faulted anticline  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1970,null,null,null,null,null,null,null,null,30,null,"Values from Kosters et al., 1989 (Table 37)",null,3296,1,"Values from Kosters et al., 1989 (Table 37)",270,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 37)","yes"]
[22,null,null,null,null,"Dirgin Fields","Rusk","TX",32.236100355555557,-94.612967877777777,"Average of Field from DrillingInfo",10133,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"28*0.3048","v":8.5343999999999998},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,"md",0.01,0.01,0.01,1,"Values from Kosters et al.,1989 (Table 37)",null,null,null,null,null,7,7,7,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct- structural nose  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1976,null,null,null,null,null,null," ",null,null,null,null,null,null,null,null,null,null,null,{"$f":"IF(F24=$CB$1,AD24,\" \")","v":" "},"yes"]
[10,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",8608,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"96*0.3048","v":29.260800000000003},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,"md",0.01,0.01,0.01,1,"Values from Kosters et al.,1989 (Table 37)",null,null,null,null,null,9,9,9,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-faulted anticline  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1966,null,null,null,null,null,null,null,null,null,null,null,null,4700,1,"Kosters et al., 1989 (Table 37)",248,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 37)","yes"]
[2,null,null,null,null,"Bethany East Field","Panola","TX",32.305104068749991,-94.113882062499968,"Average of Field from DrillingInfo",8110,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"180*0.3048","v":54.864000000000004},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,"md",0.1,0.1,0.1,1,"Values from Kosters et al.,1989 (Table 37)",null,null,null,null,null,8,8,8,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-facies change  strat-faulted anticline","gas an oil",null,null,null,null,null,null,null,null,null,1972,null,null,null,null,null,null,null,null,27,null,"Values from Kosters et al., 1989 (Table 37)",null,4100,1,"Values from Kosters et al., 1989 (Table 37)",245,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 37)","yes",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,{"$f":"IF($F$3=CV$1,$AD$3,\" \")","v":" "},{"$f":"IF($F$3=CW$1,$AD$3,\" \")","v":" "},{"$f":"IF($F$3=CV$1,$AD$3,\" \")","v":" "},{"$f":"IF($F$3=CY$1,$AD$3,\" \")","v":" "},{"$f":"IF($F$3=CW$1,$AD$3,\" \")","v":" "},{"$f":"IF($F$3=DA$1,$AD$3,\" \")","v":" "},{"$f":"IF($F$3=DA$1,$AD$3,\" \")","v":" "}]
[31,null,null,null,null,"Henderson North Field","Rusk","TX",32.238958799999999,-94.802898740000003,"Average of Field from DrillingInfo",10530,null,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,{"$f":"58*0.3048","v":17.6784},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,"md",0.05,0.05,0.05,1,"Values from Kosters et al., 1989 (Table 38)",null,null,null,null,null,10,10,10,1,"Values from Kosters et al., 1989 (Table 38)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct- anticline  strat- facies change","solution gas",null,"gas and oil",null,null,null,null,null,null,null,1979,null,null,null,null,null,null," ",null,20,null,"values from Kosters et al., 1989 (Table 38)",null,5600,1,"Values from Kosters et al., 1989 (Table 38)",272,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 38)","yes",{"$f":"IF(F27=$CC$1,AD27,\" \")","v":" "}]
[74,null,null,4236530760,null,"Carthage (Kyle No 2-A)","Panola","TX",32.104211999999997,-94.321529999999996,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone G",null,null,null,null,null,null,null,null,null,"md",0.05,0.05,0.05,1,"Values from Wilson, 1984",null,null,null,null,null,6.8,6.8,6.8,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[73,null,null,4236531224,null,"Carthage (Neal No 2)","Panola","TX",32.072678000000003,-94.270145999999997,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone E",null,null,null,null,null,null,null,null,null,"md",0.03,0.03,0.03,1,"Values from Wilson, 1984",null,null,null,null,null,6.9,6.9,6.9,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[72,null,null,4236531224,null,"Carthage (Neal No 2)","Panola","TX",32.072678000000003,-94.270145999999997,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone D",null,null,null,null,null,null,null,null,null,"md",0.04,0.04,0.04,1,"Values from Wilson, 1984",null,null,null,null,null,6.1,6.1,6.1,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[71,null,null,4236531224,null,"Carthage (Neal No 2)","Panola","TX",32.072678000000003,-94.270145999999997,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone C",null,null,null,null,null,null,null,null,null,"md",0.04,0.04,0.04,1,"Values from Wilson, 1984",null,null,null,null,null,5.7,5.7,5.7,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[70,null,null,4236530638,null,"Carthage (Caudle No 1)","Panola","TX",32.129584000000001,-94.259844000000001,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone G",null,null,null,null,null,null,null,null,null,"md",0.02,0.02,0.02,1,"Values from Wilson, 1984",null,null,null,null,null,6.3,6.3,6.3,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[69,null,null,4236530638,null,"Carthage (Caudle No 1)","Panola","TX",32.129584000000001,-94.259844000000001,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone F",null,null,null,null,null,null,null,null,null,"md",0.06,0.06,0.06,1,"Values from Wilson, 1984",null,null,null,null,null,8,8,8,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[68,null,null,4236530638,null,"Carthage (Caudle No 1)","Panola","TX",32.129584000000001,-94.259844000000001,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone B",null,null,null,null,null,null,null,null,null,"md",0.06,0.06,0.06,1,"Values from Wilson, 1984",null,null,null,null,null,6.4,6.4,6.4,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[67,null,null,4236530638,null,"Carthage (Caudle No 1)","Panola","TX",32.129584000000001,-94.259844000000001,"Texas Railroad Commission",null,null,"Sandstone",null,null,"Cotton Valley Sandstone","zone A",null,null,null,null,null,null,null,null,null,"md",0.33,0.33,0.33,1,"Values from Wilson, 1984",null,null,null,null,null,8.1,8.1,8.1,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[66,null,null,4236530251,null,"Carthage (Williamson No.3)","Panola","TX",32.097681999999999,-94.226186999999996,"USGS 7.5 min Quadrangle map",9026,9087,"Sandstone",null,null,"Cotton Valley Sandstone","zone F",null,null,null,null,null,null,null,null,null,"md",0.04,0.04,0.04,1,"Values from Wilson, 1984",null,null,null,null,null,5.8,5.8,5.8,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[65,null,null,4236530251,null,"Carthage (Williamson No.3)","Panola","TX",32.097681999999999,-94.226186999999996,"USGS 7.5 min Quadrangle map",8532,8806,"Sandstone",null,null,"Cotton Valley Sandstone","zone B",null,null,null,null,null,null,null,null,null,"md",0.04,0.04,0.04,1,"Values from Wilson, 1984",null,null,null,null,null,6.3,6.3,6.3,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[64,null,null,4236530251,null,"Carthage (Williamson No.3)","Panola","TX",32.097681999999999,-94.226186999999996,"USGS 7.5 min Quadrangle map",8427,8532,"Sandstone",null,null,"Cotton Valley Sandstone","zone A",null,null,null,null,null,null,null,null,null,"md",0.03,0.03,0.03,1,"Values from Wilson, 1984",null,null,null,null,null,6.2,6.2,6.2,1,"Values and Uncertainty from Wilson, 1984| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Wilson, 1984",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"joe"]
[37,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",4040,null,"Limestone",null,null,"Glen Rose Limestone",null,null,{"$f":"36*0.3048","v":10.972800000000001},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"struct- anticline-dome",null,null,"gas and oil",null,null,null,null,null,null,null,1949,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[9.1999999999999993,null,null,null,null,"Carthage Field N","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",3762,null,"Limestone",null,null,"Glen Rose Limestone",null,null,{"$f":"32*0.3048","v":9.7536000000000005},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"structural (anticline)",null,null,"gas",null,null,null,null,null,null,null,1966,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[32,null,null,null,null,"Willow Springs Field","Gregg","TX",32.521326640970337,-94.78636420539091,"Average of Field from DrillingInfo",6807,null,"Limestone",null,null,"Henderson Limestone",null,null,{"$f":"25*0.3048","v":7.62},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural (anticline)",null,null,"gas",null,null,null,null,null,null,null,1952,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[51,null,null,null,null,"Overton North Field","Rusk","TX",32.198692900000005,-95.022466399999999,"Average of Field from DrillingInfo",7841,7850,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"0.3048*6.1","v":1.85928},1,"Average pay from Jasper and Berkoben, 1989",null,null,null,null,null,"md",500,0,250,5,"Mathematical mean of values taken form Jasper and Berkoben, 1989",null,null,null,null,null,18,6,{"$f":"(18+6)/2","v":12},5,"Mean of values from Jasper and Berkoben | Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Jasper and Berkoben, 1989",null,null,null,"stratigraphic","solution gas drive",null,"oil and gas",null,null,null,null,null,null,null,"1979-06-03",null,null,null,null,null,null,null,null,"18.5-47",null,"Values from Jasper and Berkoben 1989",null,3723,1,"IBHSIP Values from Jasper and Berkoben 1989",230,"Farhenheit",1,"Values from Jasper and Berkoben 1989","yes",{"$f":"IF(F42=$CC$1,AD42,\" \")","v":" "}]
[25,null,null,null,null,"Hallsville Northeast Field","Harrison","TX",32.609736746153871,-94.417736217948757,"Average of Field from DrillingInfo",6522,6897,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"7.3*0.3048","v":2.2250399999999999},1,"Values from Jones, 1964",null,null,null,null,null,"md",31.7,31.7,31.7,1,"Values from Jones, 1964",null,null,null,null,null,15.8,15.8,15.8,1,"Values from Jones, 1964| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Jones, 1964",null,null,null,"stratigraphic","gas solution ",null,"oil and gas",null,null,null,null,null,null,null,1956,null,null,null,null,null,null,null,null,24.9,null,"Values from Jones, 1964",null,2846,1,"IBHSIP Values from Jones 1964",null,null,null,{"$f":"IF(F43=$CB$1,AD43,\" \")","v":" "},"yes",{"$f":"IF(F43=$CC$1,AD43,\" \")","v":" "}]
[6,null,null,null,null,"Bethany Field","Panola","TX",32.355473518013092,-94.187289781222688,"Average of Field from DrillingInfo",5800,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"34*0.3048","v":10.363200000000001},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,"md",17,5,8,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,16,16,16,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural-stratigraphic (faulted anticline and facies change)","solution gas",null,"gas",null,null,null,null,null,null,null,1948,null,null,null,null,null,null,null,null,null,null,null,null,2720,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,{"$f":"IF(F44=$CB$1,AD44,\" \")","v":" "},"yes",{"$f":"IF(F44=$CC$1,AD44,\" \")","v":" "}]
[5,null,null,null,null,"Bethany Field","Panola","TX",32.355473518013092,-94.187289781222688,"Average of Field from DrillingInfo",6130,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"19*0.3048","v":5.7911999999999999},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,"md",40,40,40,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,15,15,15,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural-stratigraphic (faulted anticline and facies change)","Pressure Depletion",null,"gas",null,null,null,null,null,null,null,1948,null,null,null,null,null,null,null,null,34,null,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,{"$f":"IF(F45=$CB$1,AD45,\" \")","v":" "},"yes",{"$f":"IF(F45=$CC$1,AD45,\" \")","v":" "}]
[9,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",6050,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"34*0.3048","v":10.363200000000001},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,"md",110,2,35,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,18,18,18,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"struct-anticline,dome  strat- facies change","Pressure Depletion",null,"gas and oil",null,null,null,null,null,null,null,1942,null,null,null,null,null,null,null,null,10,null,"Values from Kosters et al., 1989 (Table 40)",null,3265,1,"Values from Kosters et al., 1989 (Table 40)",209,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 40)","yes",{"$f":"IF(F46=$CC$1,AD46,\" \")","v":" "}]
[9.1,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",5870,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"10*0.3048","v":3.048},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,"md",94,1.4,20,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,17,17,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,null,null,null,null,"structural-stratigraphic (anticline and facies change)","Pressure Depletion",null,"gas",null,null,null,null,null,null,null,1936,null,null,null,null,null,null,null,null,30,null,"Values from Kosters et al., 1989 (Table 40)",null,3085,1,"Values from Kosters et al., 1989 (Table 40)",207,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 40)","yes"]
[79,null,null,null,null,"Hallsville South Field","Harrison","TX",32.394073473333336,-94.47491800666667,"Average of Field from DrillingInfo",6536,null,"Limestone",null,null,"Pettet Limestone",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"stratigraphic (facies change)",null,null,"gas",null,null,null,null,null,null,null,1952,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[19,null,null,null,null,"Scottsville North Field","Harrison","TX",32.543165872727265,-94.151063290909079,"Average of Field from DrillingInfo",6173,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"14*0.3048","v":4.2671999999999999},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"stratigraphic (facies change)",null,null,"gas",null,null,null,null,null,null,null,1954,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[17,null,null,null,null,"Waskom Field","Harrison","TX",32.469260472356183,-94.126346337569501,"Average of Field from DrillingInfo",6000,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"11*0.3048","v":3.3528000000000002},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural (anticline)",null,null,"gas",null,null,null,null,null,null,null,1949,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[40,null,null,null,null,"Waskom Field","Harrison","TX",32.469260472356183,-94.126346337569501,"Average of Field from DrillingInfo",5635,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"49*0.3048","v":14.9352},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural (anticline)",null,null,"gas",null,null,null,null,null,null,null,1950,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[81,null,null,null,null,"Woodlawn Field","Harrison","TX",32.647414041089128,-94.334453307095743,"Average of Field from DrillingInfo",6500,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"6*0.3048","v":1.8288000000000002},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,"md",120,3,74,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,13,13,13,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural-stratographic (structural nose and facies change)","solution gas and gas-cap expansion",null,null,null,null,null,null,null,null,null,1951,null,null,null,null,null,null,null,null,18,null,"Values from Kosters et al., 1989 (Table 40)",null,3075,1,"Values from Kosters et al., 1989 (Table 40)",null,null,{"$f":"IF(F52=$CA$1,AD52,\" \")","v":" "},{"$f":"IF(F52=$CB$1,AD52,\" \")","v":" "},"yes",{"$f":"IF(F52=$CC$1,AD52,\" \")","v":" "}]
[20,null,null,null,null,"Danville Field","Rusk","TX",32.390292283161493,-94.80537202714774,"Average of Field from DrillingInfo",7381,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"10*0.3048","v":3.048},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,"md",110,110,110,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,null,null,16,16,16,1,"Values from Kosters et al., 1989 (Table 41)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural-stratographic (structural nose and facies change)",null,null,"gas",null,null,null,null,null,null,null,1959,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,232,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 41)","yes",{"$f":"IF(F53=$CC$1,AD53,\" \")","v":" "}]
[29,null,null,null,null,"Henderson Field","Rusk","TX",32.211088220000001,-94.825137609999999,"Average of Field from DrillingInfo",7280,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"15*0.3048","v":4.5720000000000001},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,"md",300,1,72,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,null,null,13,13,13,1,"Values from Kosters et al., 1989 (Table 41)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural (anticline)","gas-cap expansion",null,"gas",null,null,null,null,null,null,null,1943,null,null,null,null,null,null,null,null,27,null,"Values from Kosters et al., 1989 (Table 41)",null,3492,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,{"$f":"IF(F54=$CB$1,AD54,\" \")","v":" "},"yes",{"$f":"IF(F54=$CC$1,AD54,\" \")","v":" "}]
[34,null,null,null,null,"Lansing North Field","Harrison","TX",32.594951171999995,-94.659098197599945,"Average of Field from DrillingInfo",7274,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"32*0.3048","v":9.7536000000000005},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural-stratigraphic (anticline and facies change)",null,null,"gas",null,null,null,null,null,null,null,1958,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[14,null,null,null,null,"Shiloh Field","Rusk","TX",32.020510893939395,-94.670221169696944,"Average of Field from DrillingInfo",7297,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"9*0.3048","v":2.7432000000000003},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural-stratigraphic (faulted anticline and facies change)",null,null,"gas",null,null,null,null,null,null,null,1960,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[38,null,null,null,null,"Willow Springs Field","Gregg","TX",32.521326640970337,-94.78636420539091,"Average of Field from DrillingInfo",7354,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"40*0.3048","v":12.192},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural (anticline)",null,null,"gas",null,null,null,null,null,null,null,1955,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[23,null,null,null,null,"Ezim Field","Rusk","TX",31.870808174999997,-94.880156639999981,"Average of Field from DrillingInfo",7856,8008,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"4*0.3048","v":1.2192000000000001},1,"Pay from Mize, 1989",null,null,null,null,null,"md",2000,50,975,5,"Mathematical mean of values from Mize, 1989",null,null,null,null,null,23,15,{"$f":"(AM58+AN58)/2","v":19},5,"Mean of values from Mize, 1989| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Mize, 1989",null,null,null,"stratigraphic","gas expansion",null,"oil and gas",null,0.91,null,null,null,null,null,"1981-02-18",null,null,null,null,null,null,null,null,"25-50",null,"Values from Mize, 1989",null,3963,1,"IFHSIP Values from Mize, 1989",null,"Farhenheit",1,"Values from Mize, 1989","yes",{"$f":"IF(F58=$CC$1,AD58,\" \")","v":" "}]
[76,null,null,null,null,"Willow Springs Field","Gregg","TX",32.521326640970337,-94.78636420539091,"Average of Field from DrillingInfo",null,null,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"30*0.3048","v":9.1440000000000001},1,"Value from Scurlock 1949",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Lenticular porosity",null,null,"Scurlock, 1949",null,null,null,"Anticline",null,null,null,null,{"$f":"35*0.3048","v":10.668000000000001},null,null,null,null,null,1938,null,null,null,null,null,null,null,null,null,"Negligible amt. ",null,null,null,null,null,null,null,null,null,"yes"]
[21,null,null,null,null,"Danville Field","Gregg and Rusk","TX",32.390292283161493,-94.80537202714774,"Average of Field from DrillingInfo",7204,7300,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"16*0.3048","v":4.8768000000000002},1,"Average pay from Snell and Robbins, 1989",null,null,null,null,null,"md",819,0.01,19.600000000000001,1,"Values from Snell and Robbins, 1989",null,null,null,null,null,21.4,8,13.5,1,"Values from Snell and Robbins, 1989|Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Snell and Robbins, 1989",null,null,null,"structural-stratigraphic","gas solution and water drive from east flowing in at 6858 ft (2090 m)",null,"gas and oil","Small to moderate acid treatment",null,null,null,null,null,null,"1960-03-13",null,null,null,null,null,null,null,null,"31-50",null,"Value from Snell and Robbins, 1989",null,3580,1,"IFHSIP Value from Snell and Robbins, 1989",232,"Farhenheit",1,"Value from Snell and Robbins, 1989","yes",{"$f":"IF(F60=$CC$1,AD60,\" \")","v":" "}]
[75,null,null,null,null,"Woodlawn Field","Harrison","TX",32.647414041089128,-94.334453307095743,"Average of Field from DrillingInfo",6280,6575,"Limestone",null,null,"Pettet Limestone",null,null,{"$f":"24*0.3048","v":7.3152000000000008},1,"From cross-section in Tefft, 1950 and production thickness",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Tefft, 1950",null,null,null,null,null,"NO Water Produced",null,null,{"$f":"279*0.3048","v":85.039200000000008},null,null,null,null,null,1949,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[57,null,null,null,null,"Marshall Field","Harrison","TX",32.621785000000003,-94.345211000000006,"Estimated on Google Maps using location description from Marshall Field Report (Teft, 1950)",6400,6650,"Limestone",null,null,"Pettet Limestone",null,null,83.2,1,"From cross-section in Tefft, 1950 and production thickness",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"streaks",null,null,null,null,null,null,null,"Tefft, 1950",null,null,null,null,null,"none",null,null,{"$f":"273*0.3048","v":83.210400000000007},null,null,null,null,null,1945,null,null,null,null,null,"none",null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[39,null,null,null,null,"Bethany Field","Panola","TX",32.355473518013092,-94.187289781222688,"Average of Field from DrillingInfo",4700,null,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":"40*0.3048","v":12.192},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural-stratigraphic (faulted anticline and facies change)","Pressure Depletion",null,"gas",null,null,null,null,null,null,null,1948,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[7,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",4900,null,"Limestone",null,null,"Rodessa Limestone","Hill Limestone",null,{"$f":"14*0.3048","v":4.2671999999999999},1," Net pay from Kosters et al., 1989 (table 40)",null,null,null,null,null,"md",200,5.3,87,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,21,21,21,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"struct-anticline,dome","Pressure Depletion",null,"gas and oil",null,null,null,null,null,null,null,1936,null,null,null,null,null,null,null,null,20,null,"Values from Kosters et al., 1989 (Table 40)",null,2636,1,"Values from Kosters et al., 1989 (Table 40)",186,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 40)","yes",{"$f":"IF(F64=$CC$1,AD64,\" \")","v":" "}]
[53,null,null,null,null,"Pine Hill S.E. Field","Panola","TX",32.09194071929825,-94.5794541982456,"Average of Field from DrillingInfo",5858,null,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":"5*0.3048","v":1.524},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,"md",100,100,100,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,17,17,17,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"stratigraphic (facies change)",null,null,"gas",null,null,null,null,null,null,null,1979,null,null,null,null,null,null,null,null,19,null,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,174,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 40)","yes",{"$f":"IF(F65=$CC$1,AD65,\" \")","v":" "}]
[60,null,null,null,null,"Waskom Field","Harrison","TX",32.469260472356183,-94.126346337569501,"Average of Field from DrillingInfo",4830,null,"Limestone",null,null,"Rodessa Limestone",null,"Hill",null,null,null,null,null,null,null,null,"md",20,20,20,1,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,14,14,14,1,"Values from Kosters et al., 1989 (Table 40)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural-stratigraphic (anticline and facies change)",null,null,"gas",null,null,null,null,null,null,null,1947,null,null,null,null,null,null,null,null,25,null,"Values from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,{"$f":"IF(F66=$CA$1,AD66,\" \")","v":" "},{"$f":"IF(F66=$CB$1,AD66,\" \")","v":" "},"yes",{"$f":"IF(F66=$CC$1,AD66,\" \")","v":" "}]
[16,null,null,null,null,"Woodlawn Field","Harrison","TX",32.647414041089128,-94.334453307095743,"Average of Field from DrillingInfo",5692,null,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":"11*0.3048","v":3.3528000000000002},1,"Net pay from Kosters et al., 1989 (Table 40)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 40)",null,null,null,"structural-stratographic (structural nose and facies change)",null,null,null,null,null,null,null,null,null,null,1951,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[36,null,null,null,null,"Lansing North Field","Harrison","TX",32.594951171999995,-94.659098197599945,"Average of Field from DrillingInfo",6734,null,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":"15*0.3048","v":4.5720000000000001},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,"md",148,0.1,15,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,null,null,14,14,14,1,"Values from Kosters et al., 1989 (Table 41)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural-stratigraphic (faulted anticline and facies change)","Pressure Depletion",null,"gas",null,null,null,null,null,null,null,1945,null,null,null,null,null,null,null,null,null,null,null,null,3191,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,{"$f":"IF(F68=$CB$1,AD68,\" \")","v":" "},"yes",{"$f":"IF(F68=$CC$1,AD68,\" \")","v":" "}]
[54,null,null,null,null,"Pone Field","Rusk","TX",32.089612495833322,-94.829868188888852,"Average of Field from DrillingInfo",6552,null,"Limestone",null,null,"Rodessa Limestone","Gloyd Limestone",null,{"$f":"5*0.3048","v":1.524},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,"md",166,166,166,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,null,null,15,15,15,1,"Values from Kosters et al., 1989 (Table 41)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"stratigraphic (facies change)",null,null,"gas",null,null,null,null,null,null,null,1959,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,200,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 41)","yes",{"$f":"IF(F69=$CC$1,AD69,\" \")","v":" "}]
[80,null,null,null,null,"Whelan Field","Harrison","TX",32.68928957923498,-94.595708636065567,"Average of Field from DrillingInfo",6776,null,"Limestone",null,null,"Rodessa Limestone",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural-stratigraphic (anticline and facies change)",null,null,"gas",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,2986,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,null,"yes"]
[63,null,null,null,null,"Willow Springs Field","Gregg","TX",32.521326640970337,-94.78636420539091,"Average of Field from DrillingInfo",6750,null,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":"20*0.3048","v":6.0960000000000001},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,"md",69,0.01,38,1,"Values from Kosters et al., 1989 (Table 41)",null,null,null,null,null,12,12,12,1,"Values from Kosters et al., 1989 (Table 41)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"structural (anticline)","Pressure Depletion",null,"gas",null,null,null,null,null,null,null,1941,null,null,null,null,null,null,null,null,25,null,"Values from Kosters et al., 1989 (Table 41)",null,null,null,null,null,null,{"$f":"IF(F71=$CA$1,AD71,\" \")","v":" "},{"$f":"IF(F71=$CB$1,AD71,\" \")","v":" "},"yes",{"$f":"IF(F71=$CC$1,AD71,\" \")","v":" "}]
[1,null,null,null,null,"Shady Lane Field","Harrison","TX",32.515699903571438,-94.341452357142856,"Average of Field from DrillingInfo",5981,5986,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":"3*0.3048","v":0.9144000000000001},1,"Average pay from Seewald, 1989",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,20,6,{"$f":"(20+6)/2","v":13},5,"Mean value calculated from values in Seewald, 1989| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Seewald, 1989",null,null,null,"stratigraphic","Pressure Depletion",null,"gas","acidized",0.91,26,null,null,null,null,"1985-08-09",null,null,null,null,null,null,null,null,43,null,"Value from Seewald, 1989",null,2450,1,"Value from Seewald, 1989",182,"Farhenheit",1,"Value from Seewald, 1989","yes"]
[56,null,null,null,null,"Tip Field","Rusk","TX",32.022707254545452,-94.844576900000007,"Average of Field from DrillingInfo",6650,6750,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":"4*0.3048","v":1.2192000000000001},1,"Average pay from Shoemaker, 1989",null,null,null,null,null,"md",10,4,4,1,"Values from Shoemaker, 1989",null,null,null,null,null,15,6,11,1,"Values from Shoemaker, 1989|Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Shoemaker, 1989",null,null,null,"stratigraphic","depletion drive",null,"oil and gas","acidized",null,null,1,"southern border along Mt. enterprise fault system","normal",null,"1985-01-04",null,null,null,null,null,null,null,null,20,null,"Values from Shoemaker, 1989",null,2794,1,"IBHSIP Values from Shoemaker, 1989",205,"Farhenheit",1,"Values from Shoemaker, 1989","yes",{"$f":"IF(F73=$CC$1,AD73,\" \")","v":" "}]
[55,null,null,null,null,"Scoober Creek Field","Rusk","TX",32.036504842105266,-94.926919687719291,"Average of Field from DrillingInfo",6840,7090,"Limestone",null,null,"Rodessa Limestone",null,null,{"$f":" 8*0.3048","v":2.4384000000000001},1,"Average pay from Shoemaker, 1989",null,null,null,null,null,"md",20,4,4,1,"Values from Shoemaker, 1989",null,null,null,null,null,21,6,12,1,"Values from Shoemaker, 1989|Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Shoemaker, 1989",null,null,null,"stratigraphic","depletion drive",null,"oil and gas","acidized",null,null,1,"southern border along Mt. enterprise fault system","normal",null,"1971-09-27",null,null,null,null,null,null,null,null,20,null,"Values from Shoemaker, 1989",null,3563,1,"IBHSIP Values from Shoemaker, 1989",215,"Farhenheit",1,"Values from Shoemaker, 1989","yes",{"$f":"IF(F74=$CC$1,AD74,\" \")","v":" "}]
[18,null,null,null,null,"Scoober Creek Field","Rusk","TX",32.036504842105266,-94.926919687719291,"Average of Field from DrillingInfo",6913,null,"Sandstone",null,null,"Rodessa Sandstone",null,null,{"$f":"13*0.3048","v":3.9624000000000001},1,"Net pay from Kosters et al., 1989 (Table 41)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 41)",null,null,null,"stratigraphic (facies change)",null,null,"gas",null,null,null,null,null,null,null,1971,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[49,null,null,null,null,"Oak Hilll Field","Rusk","TX",32.331712323036847,-94.673940260897368,"Average of Field from DrillingInfo",null,null,"Sandstone",null,null,"Taylor Sandstone",null,null,null,null,null,null,null,null,null,null,"md",0.06,0.06,0.06,1,"Values from Vavra, 1991",null,null,null,null,null,6.1,6.1,6.1,1,"Values from Vavra, 1991|Uncertainty 1=empirical related to formation 5=assigned from calc.","Permeanbility - air, Porosity - Helium",null,"Vavra, 1991",null,null,"Quartz",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,35,null,null,null,null,null,null,null,null,{"$f":"IF(F76=$CA$1,AD76,\" \")","v":" "},{"$f":"IF(F76=$CB$1,AD76,\" \")","v":" "},"yes",{"$f":"IF(F76=$CC$1,AD76,\" \")","v":" "}]
[35,null,null,null,null,"Lansing North Field","Harrison","TX",32.594951171999995,-94.659098197599945,"Average of Field from DrillingInfo",7328,8003,"Sandstone",null,"Limestone","Travis Peak Sandstone",null,null,{"$f":" (M77-L77)*0.3048","v":205.74},1,"Top and bottom depths from cross-section in Schoeneck ",null,null,null,null,null,"md",77,0,{"$f":"(AC77+AD77)/2","v":38.5},1,"horizontal higher (ave for hor)/ vertical = 53.6",null,null,null,"extremely variable",null,15,1,{"$f":"(AM77+AN77)/2","v":8},5,"Values from text of Schoeneck",null,null," Schoeneck, 1950",null,null,"Calcium Carbonate","structural-convex ",null,null,null,null,12.2,null,null,null,null,null,1949,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,{"$f":"IF(F77=$CB$1,AD77,\" \")","v":" "},"yes"]
[15,null,null,null,null,"Cyril Field","Rusk","TX",32.198870624000001,-94.834312420000003,"Average of Field from DrillingInfo",7530,7650,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"14*0.3048","v":4.2671999999999999},1,"Average pay from Clawson, 1989",null,null,null,null,null,"md",200,1,100,5,"Values from Clawson 1989",null,null,null,null,null,18,9,{"$f":"(AM78+AN78)/2","v":13.5},5,"Mean of values from Clawson 1989| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Clawson, 1989",null,null,"Quartz","stratigraphic","solution gas drive",null,"oil and gas","acidized",null,null,null,null,null,null,"1963-04-01",null,null,null,null,null,null,null,null,"25-55",null,"Values from Clawson 1989",null,3550,1,"IBHSIP Values from Clawson 1989",200,"Farhenheit",1,"Values from Clawson 1989","yes",{"$f":"IF(F78=$CC$1,AD78,\" \")","v":" "}]
[59,null,null,null,null,"Waskom Field","Harrison","TX",32.469260472356183,-94.126346337569501,"Average of Field from DrillingInfo",7404,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"36*0.3048","v":10.972800000000001},1,"Net pay from Kosters et al.,1989 (table 37)",null,null,null,null,null,"md",65,65,65,1,"Values from Kosters et al., 1989 (Table 37)",null,null,null,null,null,17,17,17,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct anticline,dome  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1973,null,null,null,null,null,null,null,null,23,null,"Values from Kosters et al., 1989 (Table37)",null,2795,1,"Values from Kosters et al., 1989 (Table 37)",198,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 37)","yes"]
[50,null,null,null,null,"Waskom Field","Harrison","TX",32.469260472356183,-94.126346337569501,"Average of Field from DrillingInfo",6053,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"107*0.3048","v":32.613599999999998},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct anticline,dome  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1947,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[13,null,null,null,null,"Carthage Field","Panola","TX",32.108370854264145,-94.32012383051844,"Average of Field from DrillingInfo",6230,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"8*0.3048","v":2.4384000000000001},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,15,15,15,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-anticline dome",null,null,"gas and oil",null,null,null,null,null,null,null,1945,null,null,null,null,null,null,null,null,null,null,null,null,3350,null,null,null,null,null,null,"yes"]
[3,null,null,null,null,"Bethany Field","Panola","TX",32.355473518013092,-94.187289781222688,"Average of Field from DrillingInfo",6300,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"15*0.3048","v":4.5720000000000001},1,"Net pay from Kosters et al., 1989 (Table 37)",null,null,null,null,null,"md",115,115,115,1,"Values from Kosters et al., 1989 (Table 37)",null,null,null,null,null,16,16,16,1,"Values from Kosters et al., 1989 (Table 37)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 37)",null,null,null,"struct-facies change  strat-faulted anticline",null,null,"oil and gas",null,null,null,null,null,null,null,1948,null,null,null,null,null,null,null,null,34,null,"Values from Kosters et al., 1989 (Table 37)",null,3113,1,"Values from Kosters et al., 1989 (Table 37)",206,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 37)","yes"]
[12,null,null,null,null,"Danville Field","Rusk","TX",32.390292283161493,-94.80537202714774,"Average of Field from DrillingInfo",7606,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"8*0.3048","v":2.4384000000000001},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"structural-stratigraphic (faulted anticline and facies change)",null,null,"oil and gas",null,null,null,null,null,null,null,1959,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[28,null,null,null,null,"Henderson Field","Rusk","TX",32.211088220000001,-94.825137609999999,"Average of Field from DrillingInfo",7457,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"18*0.3048","v":5.4864000000000006},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,"md",72,72,72,1,"Values from Kosters et al., 1989 (Table 38)",null,null,null,null,null,18,18,18,1,"Values from Kosters et al., 1989 (Table 38)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct-anticline",null,null,"gas and oil",null,null,null,null,null,null,"                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                                     ",1950,null,null,null,null,null,null,null,null,26,null,"Values from Kosters et al., 1989 (Table 38)",null,3186,1,"Values from Kosters et al., 1989 (Table 38)",185,"Farhenheit",1,"Values from Kosters et al., 1989 (Table 38)","yes",{"$f":"IF(F84=$CC$1,AD84,\" \")","v":" "}]
[30,null,null,null,null,"Henderson South Field","Rusk","TX",32.118186153846153,-94.781991348717966,"Average of Field from DrillingInfo",7450,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"24*0.3048","v":7.3152000000000008},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct- faulted anticline strat- facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1943,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[4,null,null,null,null,"Henderson South Field","Rusk","TX",32.118186153846153,-94.781991348717966,"Average of Field from DrillingInfo",7414,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"4*0.3048","v":1.2192000000000001},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct- structural nose  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1965,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[62,null,null,null,null,"Lansing North Field","Harrison","TX",32.594951171999995,-94.659098197599945,"Average of Field from DrillingInfo",7906,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"430*0.3048","v":131.06399999999999},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,10,10,10,1,"Values from Kosters et al., 1989 (Table 38)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"structural-stratigraphic (anticline and facies change)",null,null,"oil and gas",null,null,null,null,null,null,null,1977,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[24,null,null,null,null,"Minden Field","Rusk","TX",32.103579120154087,-94.7431330210525,"Average of Field from DrillingInfo",7372,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"15*0.3048","v":4.5720000000000001},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct-nose  strat-facies change",null,null,"gas and oil",null,null,null,null,null,null,null,1953,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"yes"]
[61,null,null,null,null,"Whelan Field","Harrison","TX",32.68928957923498,-94.595708636065567,"Average of Field from DrillingInfo",7322,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"474*0.3048","v":144.4752},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,"md",83,0.05,{"$f":"(AC89+AD89)/2","v":41.524999999999999},5,"Mathematical mean of values from Kosters et al., 1989 (Table 38)",null,null,null,null,null,13,13,13,1,"Values from Kosters et al., 1989 (Table 38)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct- anticline-dome","Pressure Depletion",null,"gas and oil",null,null,null,null,null,null,null,1946,null,null,null,null,null,null,null,null,33,null,"values from Kosters et al., 1989 (Table 38)",null,null,null,null,null,null,{"$f":"IF(F89=$CA$1,AD89,\" \")","v":" "},{"$f":"IF(F89=$CB$1,AD89,\" \")","v":" "},"yes",{"$f":"IF(F89=$CC$1,AD89,\" \")","v":" "}]
[77,null,null,null,null,"Willow Springs Field","Gregg","TX",32.521326640970337,-94.78636420539091,"Average of Field from DrillingInfo",7638,null,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"226*0.3048","v":68.884799999999998},1,"Net pay from Kosters et al., 1989 (Table 38)",null,null,null,null,null,"md",20,20,20,1,"Values from Kosters et al., 1989 (Table 38)",null,null,null,null,null,13,13,13,1,"Values from Kosters et al., 1989 (Table 38)| Uncertainty 1=empirical related to formation 5=assigned from calc.",null,null,"Kosters et al., 1989 (Table 38)",null,null,null,"struct-anticline",null,null,"gas and oil",null,null,null,null,null,null,null,1954,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,{"$f":"IF(F90=$CA$1,AD90,\" \")","v":" "},{"$f":"IF(F90=$CB$1,AD90,\" \")","v":" "},"yes",{"$f":"IF(F90=$CC$1,AD90,\" \")","v":" "}]
[23.1,null,null,null,null,"Ezim Field","Rusk","TX",31.870808174999997,-94.880156639999981,"Average of Field from DrillingInfo",8064,8258,"Sandstone",null,null,"Travis Peak Sandstone",null,null,{"$f":"60*0.3048","v":18.288},1,"Pay from Mize, 1989",null,null,null,null,null,"md",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,"Mize, 1989",null,null,null,"stratigraphic",null,null,"oil and gas",null,null,null,null,null,null,null,"1984",null,null,null,null,null,null,null,null,null,null,null,null,980,1,"BFHSIP Values from Mize, 1989",225,"Farhenheit",1,"Values from Mize, 1989","yes-new",{"$f":"IF(F91=$CC$1,AD91,\" \")","v":" "}]
[83,null,null,null,null,"model-1","10 km area","TX",null,null,null,null,8900,"Sandstone",null,null,"Travis Peak Sandstone",null,null,550,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,"md",200,80,90,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,18,14,15,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,30,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",206,"Farhenheit",1,"Average value from above","Maria"]
[84,null,null,null,null,"model-2","10 km area","TX",null,null,null,null,8900,"Sandstone",null,null,"Travis Peak Sandstone",null,null,382.92682926829269,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,"md",90,50,65,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,15,10,13,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,20,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",200,"Farhenheit",1,"Average value from above","Maria"]
[85,null,null,null,null,"model-3","10 km area","TX",null,null,null,null,8900,"Sandstone",null,null,"Travis Peak Sandstone",null,null,200,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,"md",20,10,15,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,10,7,8,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,10,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",185,"Farhenheit",1,"Average value from above","Maria"]
[86,null,null,null,null,"model-4","10 km area","TX",null,null,null,null,11000,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,450,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,"md",6,3,4,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,12,12,12,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,30,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",270,"Farhenheit",1,"Average value from above","Maria"]
[87,null,null,null,null,"model-5","10 km area","TX",null,null,null,null,11000,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,120,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,"md",4,0.2,0.3,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,8,6,7,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,20,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",260,"Farhenheit",1,"Average value from above","Maria"]
[88,null,null,null,null,"model-6","10 km area","TX",null,null,null,null,11000,"Sandstone",null,null,"Cotton Valley Sandstone",null,null,25,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,"md",0.01,0.01,0.01,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,2,1,2,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,10,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",245,"Farhenheit",1,"Average value from above","Maria"]
[89,null,null,null,null,"model-7","10 km area","TX",null,null,null,null,6000,"Sandstone",null,null,"Pettet Limestone",null,null,100,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,"md",1000,750,900,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,23,20,21,1,"Depth for model Maximum calc from RRC Formation tops",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,30,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",230,"Farhenheit",1,"Average value from above","Maria"]
[90,null,null,null,null,"model-8","10 km area","TX",null,null,null,null,6000,"Sandstone",null,null,"Pettet Limestone",null,null,38,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,"md",200,75,110,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,17,12,14,1,"Depth for model Average calc from fluid injection well perforations - DrillingInfo spreadsheet",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,20,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",222,"Farhenheit",1,"Average value from above","Maria"]
[91,null,null,null,null,"model-9","10 km area","TX",null,null,null,null,6000,"Sandstone",null,null,"Pettet Limestone",null,null,2,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,"md",10,3,4,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,12,10,11,1,"Depth for model Minimum calc from values above averaged for related formation hydrocarbon zone",null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,null,10,null,"Values given based on above values, yet in calculations for RPI and RFC the value has little impact.",null,3000,1,"Average value from above",210,"Farhenheit",1,"Average value from above","Maria"]

{"sheet":"Metadata","index":1,"n_rows":25,"n_cols":2,"rows_kept":25,"cut":false,"hidden":false,"merged":[[3,2,5,2],[6,2,7,2]]}
[null,"Metadata"]
["Title of dataset"]
["Description of dataset"]
["Author name"]
["Author role"]
["Author organization affiliation name"]
["Author e-mail address"]
["Author telephone number"]
["Author postal Address"]
["Source citation"]
["SourceMetadataURI"]
["Distributor person name"]
["Distributor position name "]
["Distributor organization affiliation name"]
["Distributor e-mail address"]
["Distributor telephone number"]
["Contact person name","Joseph Batir"]
["Contact position name "]
["Contact organization affiliation name","SMU Geothermal Laboratory"]
["Contact e-mail address","jbatir@smu.edu"]
["Contact telephone number"]
["Contact postal Address"]
["Use Constraints"]
["Notes on conventions used in this dataset"]
["DataEntrySource"]

{"sheet":"FieldList","index":2,"n_rows":82,"n_cols":8,"rows_kept":82,"cut":false,"hidden":false,"merged":[]}
["Field List",null,null,null,null,null,null,"Please follow directions in this column and element description column to fill in data in the data sheet. First look in this column, and if there is no information or it is unclear, then follow the element description information to fill in cell"]
["Interchange Content Element","Data Type","Implementation","Cardinality","Element Description","Domain","Example(s)","Notes for Shar and Harrison Pertaining to the E. Texas Project"]
["OBJECTID","int","int",1,"Added by GIS software.",null,null,"This column is not in the spreadsheet, but added in when imported into ArcGIS - do not worry about it not being there, start with worker name"]
["Worker Name","free text","string",1,"Name of work inputing information into this content model",null,null,"Put your name - the person adding in the data"]
["ObservationURI","URI","string 255",1,"Unique identifier for this observation. This is the identifier (Uniform Resource Identifier) that will be used to cross-reference data, samples, and other observations to the observation represented by this record. Best practice is to define an http URI that will dereference to a normative description of the observation. USGIN URI's may be redirected to any URL using the http://resources.usgin.org redirector; contact the USGIN development team at AZGS for instructions.",null,null,"Field will be hidden - this will be filled in later"]
["ObservationName","free text","string",1,"The human-intelligible name for the observation; may be a concatenation of observation type and feature name."]
["WellType","term","string",1,"Type of well that contains the borehole identified by the HeaderURI, at the time indicated in the StatusDate element.",null,"AB (Plugged and Abandoned); AI  (Air injection); BM  (Brine Mining); CM (Coal bed methane); CO  (CO2 injection); DH (Drill hole); DI  (Disposal); DW  (Domestic Well); EOR (Enhanced oil recovery); EX (Exploration); \nGAS (Gas)\n","Field will be hidden - this will be filled in later"]
["HeaderURI","URI","string 255",1,"Unique identifier for the borehole indicated by this record. This identifier should identify the physical well, based on the API number if available. Otherwise, the URI should incorporate one of the OtherID values. Please contact the USGIN development team at AZGS for instructions.",null,null,"INPUT THE API INTO THIS COLUMN IF DATA IS FROM A WELL"]
["WellName","string","free text","0..1","Common or human-readable name by which the feature is known. Recommend using only web-safe characters (a-z A-Z 0-9 _-.) in the name. Be consistent in the naming convention used within any given dataset.",null,null,"Field will be hidden - this will be filled in later"]
["OtherID","string","free text","0..1","Alternative identifier(s) for the feature. Indicate the authority from which the OtherID is derived with a short (lower case) prefix delimited by a colon ':' If identifiers from multiple different authorities are available, delimit these identifiers with the pipe '|' character. For example, if a well were known to the Arizona Geological Survey (AZGS) by the id number 1337, the prefix would be azgs: and the identifier string would be azgs:1337. Any such prefixes used to scope identifiers should be explained in the dataset metadata.",null,null,"IF DATA IS FROM A FIELD, INPUT FIELD NAME HERE"]
["County","free text","string",1,"Required. County name. If unknown or not applicable use 'missing'. If offshore, specify 'offshore' in this field.",null,null,"If data is well data - leave blank\nIf data is from any other source, please fill in"]
["State","free text","string",1,"Required. State name without abbreviations. If unknown or not applicable use 'missing'. For offshore locations, specify the governing or nearest state and list the county as 'offshore'.",null,null,"This field will be hidden "]
["LatDegree","decimal","double ",1,"Latitude coordinate for the surface location of the feature (use center point for areas); values should be provided with at least 4 significant digits for sufficient precision (7 decimal places is recommended by the USGS (OFR 02-463, p. 6). Use decimal degrees.",null,null,"If well - leave blank\nIf field average data - pick the center of the field as the location and input that here\nif other data, should have an associated lat/long"]
["LongDegree","decimal","double ",1,"Longitude coordinate for the surface location of the feature (use center point for areas); values should be provided with at least 4 significant digits for sufficient precision (7 decimal places is recommended by the USGS (OFR 02-463, p. 6). Use decimal degrees.",null,null,"If well - leave blank\nIf field average data - pick the center of the field as the location and input that here\nif other data, should have an associated lat/long"]
["LocationUncertaintyStatement","free text","string",1,"Information on how the original location was determined, e.g., 1:250,000 map, gps unit, Google Earth, PLSS Conversion, Spatial Datum Conversion, e.g., NAD27 to WGS84.",null,null,"State location information source (map, google earth, well header, etc.) and give type of same (rock outcrop, well, field average, etc.)"]
["DepthTopInterval_ft","decimal","double ",1,"Depth to the top of the interval, reported in feet from borehole origin. "]
["DepthBottomInterval_ft","decimal","double ",1,"Depth to the bottom of the interval, reported in feet from borehole origin."]
["RockType","free text","string",1,"Free text name for lithology category of sample, e.g. biotite-hornblende granite, lithofeldspathic sandstone, calcareous arkose, biotite schist."]
["Lithology","free text","string","0..1","Description of the lithology of surface geology or geologic column for well interval, e.g. granite, sandstone, limestone, arkose, schist. Recommend using CGI simple lithology vocabulary (see tab in this workbook). Use to account for EarthChem Material, EarthChem Type, EarthChem Composition, alluvium, 36-40': gravels; etc.",null,null,"Here, use the Simple Lithology from SimpleLithology2012.  This is the lithology of interest, i.e. sandstone, limestone, shale, etc.\nThis should be the dominant lithology of the reservoir of Interest"]
["OtherLithologyName","free text ","string","0..1","Other rock types that are constituents of the reservoir; separate names with pipe ('|') character.",null,null,"Other rock types that are constituents of the reservoir that are not the dominant lithology of interest; separate names with pipe ('|') character."]
["GeologicUnitName","free text","string",1,"Name of geologic unit that was sampled. Include hierarchy of names if the unit is part of a higher-rank geologic unit, e.g. Group name/Formation name, or Formation/Member, or Group/ Formation. Spell out unit names in full.",null,null,"Here, input the reservoir of interest - i.e. Cotton Valley, Travis Peak, etc."]
["OtherFormationName","free text ","string","0..1","Other named geologic units that are of interest to the study; separate names with pipe ('|') character.  ",null,null,"If reservoir has multiple producing layers that are named in the literature, separate those layers out here - Example - Cotton Valley group has other layers that are not just the Cotton Valley, list those here if they are mentioned in the report you are writing about"]
["PercentTargetRock","decimal","double","0..1","Target Rock (Sand, shale, etc.) volume divided by block volume. ",null,null,"Fill in for both wells and fields"]
["AverageNetTargetRockThickness_m","decimal","double","0..1","Average net target rock thickness within the reservoir/fairway boundaries identified as calculated from well log interpretation. Describe method and uncertainty in appropriate fields. ",null,null,"For wells - leave blank and we will calculate from the well logs.\nFor fields - if this data is available record it"]
["AverageNetTargetRockThicknessUncertainty","free text ","string","0..1","An expression of the confidence in the  AverageNetTargetRockThickness value.  Best practice to include units and assumptions for calculating uncertainty within AverageReservoirDepthMethodology.  ",null,null,"For wells - leave blank for now\nFor fields - there should be a ± measurement for thickness, use this"]
["AverageNetTargetRockThicknessMethodology","free text ","string","0..1","The method for well log interpretation in calculating AverageNetTargetRockThickness_m is stated here.  Required if AverageNetTargetRockThickness_m is provided.  Also include units and explanation for AverageNetTargetRockThicknessUncertainty value.  ",null,null,"Please input if the net target rock thickness is labeled at net sand thickness / net pay / reservoir thickness / etc.  "]
["VerticalConductivity_ft_day","decimal","double ","0..1","Physical property that quantitatively describes the ability of a fluid to move vertically through the pore spaces and/or fractures in a material.  Report Conductivity values in ft/day."]
["HorizontalConductivity_ft_day","decimal","double ","0..1","Physical property that quantitatively describes the ability of a fluid to move horizontally through the pore spaces and/or fractures in a material.  Report Conductivity values in ft/day."]
["SpecificStorage","decimal","double ","0..1","The volume of water an aquifer releases from or takes into storage per unit surface area of the aquifer per unit change in head."]
["UnitsStorage","string","free text","0..1","Units for the reported specific storage. (1/[length])."]
["Permeability","decimal","double ","0..1","The property or capacity of a porous rock, sediment, or soil for transmitting a fluid; it is a measure of the relative ease of fluid flow under unequal pressure."]
["UnitsPermeability","free text","string","0..1","Units for the reported permability. The SI unit for permeability is m^2. A practical unit for permeability is the darcy (D), or more commonly the millidarcy (mD) (1 darcy \\approx10−12/m^2). "]
["PermeabilityMax_m2","decimal","double","0..1","Maximum permeability based on Literature values for the field or calculated permeability using production tests. Units square meters (m2).",null,null,"If only average Permeability is available for the field, put that in for Max, Min, and Avg"]
["PermeabilityMin_m2","decimal","double","0..1","Minimum permeability based on Literature values for the field or calculated permeability using production tests. Units square meters (m2)."]
["PermeabilityAverage_m2","decimal","double","0..1","The Average Permeability available from public data sources.  The method for calculating an average should be stated in PermeabilityAverageMethod.   Where only one permeability value is obtained from public data sources, the minimum, maximum, and average will be identical."]
["PermeabilityAverageUncertainty","free text ","string","0..1","An expression of the confidence in the  PermeabilityAverage_m2 value.  Best practice to include units and assumptions for calculating uncertainty within PermeabilityAverageMethod.  "]
["PermeabilityAverageMethod","free text ","string","0..1","The method for calculating PermeabilityAverage_m2 is stated here.  Required if PermeabilityAverage_m2 is provided.  Also provide units and explanation for calculating PermeabilityAverageUncertainty.",null," Examples include:  Based upon a single published value, with a stated reference.  Weighted average of permeability values for stratigraphic column to depth, with source of stratigraphic column.  Mean average of x number of permeability values from published sources. Example of PermeabilityAverageUncertainty would include units (such as co-efficient of variation, or a letter or number scale) along with an explanation or link to more detail."]
["SpecificYield_percent","decimal","double ","0..1","The ratio of the volume of water that a given mass of saturated rock or soil will yield by gravity to the volume of that mass."]
["Transmissivity","decimal","double ","0..1","The transmissivity is a measure of how much water can be transmitted horizontally, such as to a pumping well. Transmissivity is directly proportional to horizontal hydraulic conductivity and thickness of the transmitting layer."]
["Transmissivity_units","free text","string","0..1","Units are (length)^2/Time. "]
["EffectivePorosity","decimal","double ","0..1","The percentage of pore volume or void space, or that volume within rock that can contain fluids."]
["Porosity","decimal","double","0..1","Porosity values obtained from public data sources",null,null,"Fill this in when there is not an effective porosity listed for the source"]
["PorosityMax_pct","decimal","double","0..1","Maximum porosity values obtained from public data sources.",null,null,"If only the average porosity for the field is available, put that in Max, Min, and Avg"]
["PorosityMin_pct","decimal","double","0..1","Minimum porosity values obtained from public data sources."]
["PorosityAverage_pct","decimal","double","0..1","The Average Porosity available from public data sources.  The method for calculating an average should be stated in PorosityAverageMethod.   Where only one porosity value is obtained from public data sources, the minimum, maximum, and average will be identical."]
["PorosityAverageUncertainty","free text ","string","0..1","An expression of the confidence in the  PorosityAverage_pct value.  Best practice to include units and assumptions for calculating uncertainty within PorosityAverageMethod.  "]
["PorosityAverageMethod","free text ","string","0..1","The method for calculating PorosityAverage_pct is stated here.  Required if PorosityAverage_pct is provided.  Also include units and explanation for PorosityAverageUncertainty value. ",null,"Examples include:  Based upon a single published value, with a stated reference.  Weighted average of porosity values for stratigraphic column to depth, with source of stratigraphic column.  Mean average of x number of porosity values from published sources. "]
["ObservationMethod","free text","string",1,"Text description of how the measurement was made - instrumentation, logging rate, correction or extrapolation process, how time since circulation was determined, etc. Data provider should indicate QA/QC performed on the data, including individual or institution, time frame and depth of quality check."]
["RelatedResource\n","free text","string","0..1","This may be one to many http links to resources (logs, pictures or other documents if available online. Should be an http:// address (URL)) related to the observation described in each record. Delimit multiple values with the pipe '|' character.",null,null,"\nThese links will have to be public access links at some point - if you have links to public access documents, use those\nAll references should be uploaded into Box- if there is no public access link then you can use the URL to the box location for now.\nFor any wells - include a link to the RRC website that gives details for the specific well"]
["Source","free text","string",1,"Mandatory. Short text explanation of source of information defining this feature or record; may be author-date type citation, well log, report, data files etc., but should include some indication of how digital data originated. If unpublished data, provide researcher name, date and research institution for proper citation. Separate multiple citations with pipe '|' character.",null,null,"Add reference information in parenthetical citation form. i.e. Koster et al., 1989 | Blackwell and Richards, 2004 | etc.\nIf newly interpreted by worker - add worker name, data source (i.e. well log), and date"]
["MetadataURI","URI","string255","0..1","URI identifying (and ideally dereferencing to get) a full formal metadata record for the observation report. A time series of observations may all reference the same metadata record that provides contact information and details on procedure, etc.",null,null,"THIS CELL WILL BE HIDDEN"]
["Shape","gml:PointPropertyType","gml:PointPropertyType",1,"Managed by GIS and web feature server; generated from point lat, long, srs",null,null,"THIS CELL WILL BE HIDDEN"]
["CementationMineralogy","free text ","string","0..1","Calcite, Quartz, Iron Oxides, Clay Minerals, etc."]
["Trap","free text ","string","0..1","Sealing formation or structural orientation to trap hydrocarbons."]
["Drive","free text ","string","0..1","Geopressure, dissolved gas drive, thermal expansion, etc."]
["WaterDensity_mgL","decimal","double","0..1","Indicate the water (or brine, likely) TDS (total dissolved solids). Unit of measure is mg/L.",null,null,"This is a measure of the water density if available - you should have already filled out TDS in WaterTDS_mgl"]
["CommodityOfInterest","free text ","string","0..1","The commodity of interest associated with the borehole.",null,"Coalbed Methane; Oil; OilAndGas (Mixtures of oil and combustible natural gas.); Gas (Combustible natural gas); GeothermalEnergy (fluid extracted from subsurface as medium for transporting heat from subsurface heat reservoir for use by people.); Helium; CarbonDioxide; OtherGas (Not sure if there are any other gases produced from subsurface…); Sulfur; Water, fresh; Brine; MetallicMinerals (base and precious metals); Salt (sodium chlorite); OtherEvaporite (borates, other salts.); OtherSolidMineral (Barite, anhydrite, zeolites, clay minerals, aggregate, etc.); Information (well was drilled for monitoring, making measurements,  acquiring stratigraphic information, etc.. Not specific to any particular commodity exploration or development.); Uranium (Uranium or thorium minerals); radioactive fluid (For disposal of radioactive material; assume nothing else really matters in this case…); Salt water (have to distinguish from brine); brackish water; air; LPG (Liquified Petroleum Gas); CO2; other; unknown\n"]
["Stimulation","free text ","string","0..1","A treatment performed to restore or enhance the productivity of a well.",null,"Acid Frac, Thermal Frac, Standard Frac, etc."]
["AveragePerforatedThickness_m","decimal","double","0..1","Average perforated thickness per well across field.",null,null,"Here, make sure you are looking at the perforated thickness within the formation of interest"]
["WellCount","integer","double","0..1","Number of wells contained by reservoir in question.  If AverageReservoirDepth_m is based on an average of well depths, especially important to provide the WellCount. ",null,null,"Record the number of wells within the given field\nIf you are adding information from an individual well, leave blank"]
["FaultCount","integer","double","0..1","Number of faults contained by field in question.",null,null,"Only fill in for field derived values"]
["Faulted","free text ","string","0..1","Indicate if the reservoir was bounded, or limited in size, by vertical faults. 'Yes' or 'No' may be appropriate indications.",null,null,"Only fill in for field derived values"]
["FaultType","free text ","string","0..1","Indicate general type of fault: Growth, Normal, Thrust.",null,null,"Only fill in for field derived values"]
["FaultHydraulicCharacter","free text ","string","0..1","Provide insight into whether there is fluid flow from greater depths along faults or if they are creating a trap/seal.",null,null,"Only fill in for field derived values"]
["FirstProductionDate","calendarDate","dateTime","0..1","Date for the record (of first production). Day, month and year must be specified; Excel will display using ISO 8601 date and time (yyyy-mm-ddT:hh:mm) format. If only the year is known, enter month and day as 'Jan. 1', (or '1/1/', or '1-1-', or 'January 1,'). All dates will be converted to yyyy-mm-ddThh:mm.",null,null,"Only fill in for field derived values"]
["LastProductionDate","calendarDate","dateTime","0..1","Date for the record (of last production). Day, month and year must be specified; Excel will display using ISO 8601 date and time (yyyy-mm-ddT:hh:mm) format. If only the year is known, enter month and day as 'Jan. 1', (or '1/1/', or '1-1-', or 'January 1,'). All dates will be converted to yyyy-mm-ddThh:mm.",null,null,"Only fill in for field derived values"]
["YearsInProduction","integer","double","0..1","Number of years of active production.",null,null,"Only fill in for field derived values"]
["MonthlyProduction_bbl","decimal","double","0..1","Used to estimate current pressure and most recent production history across the field.",null,null,"Only fill in for field derived values"]
["ProductionReportDate","calendarDate","dateTime","0..1","Date for monthly production value. Day, month and year must be specified; Excel will display using ISO 8601 date and time (yyyy-mm-ddT:hh:mm) format. If only the year is known, enter month and day as 'Jan. 1', (or '1/1/', or '1-1-', or 'January 1,'). All dates will be converted to yyyy-mm-ddThh:mm.",null,null,"Only fill in for field derived values"]
["AverageMonthlyWaterProduction_bbl","decimal","double","0..1","Average monthly water production for every well in the field.",null,null,"Only fill in for field derived values"]
["MinimumMonthlyWaterProduction_bbl","decimal","double","0..1","Minimum monthly water production from a well in the field.",null,null,"Only fill in for field derived values"]
["MaximumMonthlyWaterProduction_bbl","decimal","double","0..1","Maximum monthly water production from a well in the field.",null,null,"Only fill in for field derived values"]
["WaterInjection_bbl","decimal","double","0..1","Amount of water injected into a formation for disposal purposes or enhanced recovery.",null,null,"Only fill in for field derived values"]
["WaterSaturation_pct","decimal","double","0..1","Water Saturation(%)."]
["WaterTDS_mgl","decimal","double","0..1","Total Dissolved Solids. Milligrams per liter."]
["AverageInitialPressure","decimal","double"]
["AverageInitialPressure_Uncertainty","free text ","string",1]
["AverageInitialPressure_Methodology","free text ","string",1]
["AverageBHT","decimal","double","0..1","Average Bottom Hole Temperature"]
["BHT units","free text ","string",1,"Bottom Hole Temperature units"]
["AverageBHT_Uncertainty","free text ","string",1,"Uncertainty for BHT based on 1 = actual published value  &  5 = value calculated from values"]
["AverageBHT_Methodology","free text ","string",1]

{"sheet":"About","index":3,"n_rows":34,"n_cols":4,"rows_kept":34,"cut":false,"hidden":false,"merged":[[29,1,29,3],[3,1,3,3],[4,1,4,3],[5,1,5,3],[6,1,6,3],[7,1,7,3],[24,0,24,3],[25,1,25,3],[26,1,26,3],[27,1,27,3],[28,1,28,3]]}
["HydraulicProperty","typeLayerName; note this cell has a DefinedName that is the same as the worksheet tab containing the data for this feature type"]
["usgincm:Hydraulic Properties","usginKeyword"]
["Data","dataTab"]
[null,"AASG Geothermal Data: Hydraulic Property observations"]
["Version",1.1000000000000001]
["Workbook Description","This workbook is an aid for compiling data for delivery as hydraulic property observations for the National Geothermal Data System. The HydraulicPropertyObservation worksheet specifies content elements for an interchange format for data obtained from boreholes.  Fields in that spreadsheet  will become XML elements in interchange documents for WFS simple features/geothermal data web services. Typically hydraulic properties are collected during pump testing and/or laboratory analysis, and this information will be provided through a hydraulic property observation service.  The HeaderURI for a particular borehole (well for simple wells) is the cross-referencing link (foreign key) used to associate the header record, well logs, temperature measurements, and other information from a particular borehole. \n"]
["Feature Description","Hydraulic conductivity, symbolically represented as K, is a property of vascular plants, soil or rock, that describes the ease with which water can move through pore spaces or fractures. It depends on the intrinsic permeability of the material and on the degree of saturation. Saturated hydraulic conductivity, Ksat, describes water movement through saturated media.\n"]
["Editors","AZGS:  Diane Love, Esty Pape, Stephen Richard, Celia Coleman, Christy Caudill"]
[]
[]
["Revision","Comment","Person","Date"]
[0.1,"Initial draft started by copying Wisconsin data and Borehole Lithology Intervals features and deleting unrelated fields","Diane Love","2011-09-20"]
[0.2,"Added Data Revision History section (below). Updated and renamed Dataset Metadata tab. Added Review Comments tab, Field List tab. Revised field headings to be consistent with WellLog content model.","Esty Pape","2012-06-18"]
[null,"Quick look. Need to get unit abbrev in observed value field names, be consistent about SI or English units. Change sheet name.","Stephen Richard","2012-09-10"]
[1,"Added a field list, updated text","Celia Coleman","2012-10-23"]
["1.0.1","Standardized Field Descriptions on FieldList for xsd and xml; deleted DataValidTerms tab.","Esty Pape","2013-08-14"]
["1.0.1","Massive formatting changes to template.","Christy Caudill","2013-08-29"]
[1.1000000000000001,"changed LatDegreeWGS84 and LongDegreeWGS84 to \"LatDegree\" and \"LongDegree\"","Laura Bookman","2015-06-22"]
[null,"Added SimpleLithology2012 tab with Simple Lithology information, added new columns highlighted light yellow that are similar to Geologic Reservoir content model for easy cross exchange between content models","Joseph Batir ","2018-02-02"]
[null,"Added AverageInitialPressure_psi,  AverageInitialPressure_Uncertainty, AverageInitialPressure_Methodology, AverageBHT_°F, AverageBHT_Uncertainty, and AverageBHT_Methodology columns","Harrison Schumann","2018-04-25"]
["to do!","add columns for units - perm, production, temp ","Maria"]
[]
[]
[]
["Tab Descriptions"]
["About","Contains versioning and revision history."]
["Metadata","Contains information for contact person an/or entity providing the information in this spreadsheet workbook."]
["Data","Contains fields for information used to discover feature or observation of interest."]
["FieldList","Contains a data mapping for interchange formats, cardinality, formatting information and instructions for populating the content model."]
["DataRevisions: ","Location to provide feedback for data providers to implement necessary edits to the data to conform to schema conventions, but is also meant to serve as a revision history for the data."]
[]
[]
[null,"This work is licensed under a Creative Commons Attribution 3.0 Unported License."]
[null,"Copyright © Arizona Geological Survey, 2012"]

{"sheet":"SimpleLithology2012","index":4,"n_rows":267,"n_cols":4,"rows_kept":267,"cut":false,"hidden":false,"merged":[]}
["URI","prefLabel","Definition","Source"]
["http://resource.geosciml.org/classifier/cgi/lithology/acidic_igneous_material","Acidic igneous material","Igneous material with more than 63 percent SiO2.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/acidic_igneous_rock","Acidic igneous rock","Igneous rock with more than 63 percent SiO2.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/alkali-olivine_basalt","Alkali olivine basalt","Alkali olivine basalt is silica-undersaturated, characterized by the absence of orthopyroxene, absence of quartz, presence of olivine, and typically contains some feldspathoid mineral, alkali feldspar or phlogopite in the groundmass. Feldspar phenocrysts typically are labradorite to andesine in composition. Augite is rich in titanium compared to augite in tholeiitic basalt. Alkali olivine basalt is relatively rich in sodium.","http://en.wikipedia.org/wiki/Basalt, Carmichael, I.S. Turner, F.J., Verhoogen, John, 1974, Igneous petrology: New York, McGraw HIll Book Co., p.42-43."]
["http://resource.geosciml.org/classifier/cgi/lithology/alkali_feldspar_granite","Alkali feldspar granite","Granitic rock that has a plagioclase to total feldspar ratio less than 0.1. QAPF field 2.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/alkali_feldspar_rhyolite","Alkali feldspar rhyolite","Rhyolitoid in which the ratio of plagioclase to total feldspar is less than 0.1. QAPF field 2.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/alkali_feldspar_syenite","Alkali feldspar syenite","Alkali feldspar syenitic rock that contains 0-5 percent quartz and no feldspathoid in the QAPF fraction. QAPF field 6.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/alkali_feldspar_syenitic_rock","Alkali feldspar syenitic rock","Syenitoid with a plagioclase to total feldspar ratio of less than 0.1. QAPF fields 6, 6*, and 6'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/alkali_feldspar_trachyte","Alkali feldspar trachyte","Trachytoid that has a plagioclase to total feldspar ratio less than 0.1, between 0 and 5 percent quartz in the QAPF fraction, and no feldspathoid minerals. QAPF field 6.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/alkali_feldspar_trachytic_rock","Alkali feldspar trachytic rock","Trachytoid that has a plagioclase to total feldspar ratio less than 0.1. QAPF fields 6, 6', and 6*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/amphibolite","Amphibolite","Metamorphic rock mainly consisting of green, brown or black amphibole and plagioclase (including albite), which combined form 75 percent or more of the rock, and both of which are present as major constituents. The amphibole constitutes 50 percent or more of the total mafic constituents and is present in an amount of 30 percent or more, other common minerals include quartz, clinopyroxene, garnet, epidote-group minerals, biotite, titanite and scapolite.","Coutinho et al. 2007, IUGS SCMR chapter 8 (http://www.bgs.ac.uk/SCMR/)"]
["http://resource.geosciml.org/classifier/cgi/lithology/andesite","Andesite","Fine-grained igneous rock with less than 20 percent quartz and less than 10 percent feldspathoid minerals in the QAPF fraction, in which the ratio of plagioclase to total feldspar is greater 0.65.  Includes rocks defined modally in QAPF fields 9 and 10 or chemically in TAS field O2 as andesite. Basalt and andesite, which share the same QAPF fields, are distinguished chemically based on silica content, with basalt defined to contain less than 52 weight percent silica.  If chemical data are not available, the color index is used to distinguish the categories, with basalt defined to contain greater than 35 percent mafic minerals by volume or greater than 40 percent mafic minerals by weight. Typically consists of plagioclase (frequently zoned from labradorite to oligoclase), pyroxenehornblende and/or biotite. Fine grained equivalent of dioritic rock.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/anorthosite","Anorthosite","Anorthositic rock that contains between 0 and 5 percent quartz and no feldspathoid mineral in the QAPF fraction. QAPF field 10.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/anorthositic_rock","Anorthositic rock","Leucocratic phaneritic crystalline igneous rock consisting essentially of plagioclase, often with small amounts of pyroxene. By definition, colour index M is less than 10, and plagiclase to total feldspar ratio is greater than 0.9. Less than 20 percent quartz and less than 10 percent feldspathoid in the QAPF fraction. QAPF field 10, 10*, and 10'.","LeMaitre et al. 2002, This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/anthracite_coal","Anthracite","Coal that has vitrinite mean random reflectance greater than 2.0% (determined in conformance with ISO 7404-5).  Less than 12-14 percent volatiles (dry, ash free), greater than 91 percent fixed carbon (dry, ash free basis). The highest rank coal, very hard, glossy, black, with semimetallic luster, semi conchoidal fracture.","Economic Commission for Europe, Committee on Sustainable Energy- United Nations (ECE-UN), 1998, International Classification of in-Seam Coals: Energy 19, 41 pp, see also Neuendorf et al. 2005, http://en.wikipedia.org/wiki/Coal#Types_of_coal,  Eberhard Lindner, Chemie für Ingenieure, Lindner Verlag Karlsruhe, S. 258"]
["http://resource.geosciml.org/classifier/cgi/lithology/anthropogenic_material","Anthropogenic material","Material known to have artificial (human-related) origin, insufficient information to classify in more detail.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/anthropogenic_unconsolidated_material","Anthropogenic unconsolidated material","Unconsolidated material known to have artificial (human-related) origin.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/aphanite","Aphanite","Rock that is too fine grained to categorize in more detail.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/aplite","Aplite","Light coloured crystalline rock, characterized by a fine grained allotriomorphic-granular (aplitic, saccharoidal or xenomorphic) texture, typically granitic composition, consisting of quartz, alkali feldspar and sodic plagioclase.","Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/arenite","Arenite","Clastic sandstone that contains less than 10 percent matrix. Matrix is  mud-size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products) of detrital or diagenetic nature.","Pettijohn, Potter, Siever, 1972, Sand and Sandstone: New York, Springer Verlag, 681 p."]
["http://resource.geosciml.org/classifier/cgi/lithology/ash_and_lapilli","Ash and lapilli","Tephra in which less than 25 percent of fragments are greater than 64 mm in longest dimension","Schmid 1981, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/ash_breccia_bomb_or_block_tephra","Ash breccia, bomb, or block tephra","Tephra in which more than 25 percent of particles are greater than 64 mm in largest dimension. Includes ash breccia, bomb tephra and block tephra of Gillespie and Styles (1999)","Schmid 1981, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/ash_tuff_lapillistone_and_lapilli_tuff","Ash tuff, lapillistone, and lapilli tuff","Pyroclastic rock in which less than 25 percent of rock by volume are more than 64 mm in longest diameter. Includes tuff, lapilli tuff, and lapillistone.","Schmid 1981, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/basalt","Basalt","Fine-grained or porphyritic igneous rock with less than 20 percent quartz, and less than 10 percent feldspathoid minerals, in which the ratio of plagioclase to total feldspar is greater 0.65. Typically composed of calcic plagioclase and clinopyroxene, phenocrysts typically include one or more of calcic plagioclase, clinopyroxene, orthopyroxene, and olivine. Includes rocks defined modally in QAPF fields 9 and 10 or chemically in TAS field B as basalt. Basalt and andesite are distinguished chemically based on silica content, with basalt defined to contain less than 52 weight percent silica.  If chemical data are not available, the color index is used to distinguish the categories, with basalt defined to contain greater than 35 percent mafic minerals by volume or greater than 40 percent mafic minerals by weight.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/basanite","Basanite","Tephritoid that has a plagioclase to total feldspar ratio greater than 0.9, and contains more than 10 percent normative (CIPW) olivine.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/basanitic_foidite","Basanitic foidite","Foiditoid that contains less than 90 percent feldspathoid minerals in the QAPF fraction, and has a  plagioclase to total feldspar ratio that is greater than 0.5, with greater than 10 percent normative olivine.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/basic_igneous_material","Basic igneous material","Igneous material with between 45 and 52 percent SiO2.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/basic_igneous_rock","Basic igneous rock","Igneous rock with between 45 and 52 percent SiO2.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/bauxite","Bauxite","Highly aluminous material containing abundant aluminium hydroxides (gibbsite, less commonly boehmite, diaspore) and aluminium-substituted iron oxides or hydroxides and generally minor or negligible kaolin minerals, may contain up to 20 percent quartz. Commonly has a pisolitic or nodular texture, and may be cemented.","Eggleton 2001"]
["http://resource.geosciml.org/classifier/cgi/lithology/biogenic_sediment","Biogenic sediment","Sediment composed of greater than 50 percent material of biogenic origin. Because the biogenic material may be skeletal remains that are not organic, all biogenic sediment is not necessarily organic-rich.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/biogenic_silica_sedimentary_rock","Biogenic silica sedimentary rock","Sedimentary rock that consists of at least 50 percent silicate mineral material, deposited directly by biological processes at the depositional surface, or in particles formed by biological processes within the basin of deposition.","based on NADM SLTT sedimentary, Hallsworth & Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/bituminous_coal","Bituminous coal","Coal that has vitrinite mean random reflectance greater than 0.6% and less than 2.0% (determined in conformance with ISO 7404-5), or has a gross calorific value greater than 24 MJ/kg (determined in conformance with ISO 1928). Hard, black, organic rich sedimentary rock, contains less than 91 percent fixed carbon on a dry, mineral-matter-free basis, and greater  than 13-14 percent volatiles (dry, ash free). Formed from the compaction or induration of variously altered plant remains similar to those of peaty deposits.","Economic Commission for Europe, Committee on Sustainable Energy- United Nations (ECE-UN), 1998, International Classification of in-Seam Coals: Energy 19, 41 pp, see also http://en.wikipedia.org/wiki/Coal#Types_of_coal,  Eberhard Lindner, Chemie für Ingenieure, Lindner Verlag Karlsruhe, S. 258"]
["http://resource.geosciml.org/classifier/cgi/lithology/boninite","Boninite","andesitic rock that contains more than 8 percent MgO. Typically consists of phenocrysts of protoenstatite, orthopyroxene, clinopyroxene, and olivine in a glassy base full of crystallites, and exhibits textures characterisitc of rapid crystal growth.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/boulder_gravel_size_sediment","Boulder gravel size sediment^^xsd:string","Sediment containing greater than 30 percent boulder-size particles (greater than 256 mm in diameter)^^xsd:string","Wentworth size scale^^xsd:string"]
["http://resource.geosciml.org/classifier/cgi/lithology/boundstone","Boundstone","Sedimentary carbonate rock with preserved biogenic texture, whose original components were bound and encrusted together during deposition by the action of plants and animals during deposition, and remained substantially in the position of growth.","Hallsworth and Knox 1999, SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/breccia","Breccia","Coarse-grained material composed of angular broken rock fragments, the fragments typically have sharp edges and unworn corners. The fragments may be held together by a mineral cement or in a fine-grained matrix, and consolidated or nonconsolidated. Clasts may be of any composition or origin. In sedimentary environments, breccia is used for material that consists entirely of angular fragments, mostly derived from a single source rock body, as in a rock avalanche deposit, and matrix is interpreted to be the product of comminution of clasts during transport. Diamictite or diamicton is used when the material reflects mixing of rock from a variety of sources, some sub angular or subrounded clasts may be present, and matrix is pre-existing fine grained material that is not a direct product of the brecciation/deposition process.","Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/breccia_gouge_series","Breccia-gouge series","Fault material with features such as void spaces (filled or unfilled), or unconsolidated matrix material between fragments, indicating loss of cohesion during deformation. Includes fault-related breccia and gouge.","SLTTm 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/calcareous_carbonate_sediment","Calcareous carbonate sediment","Carbonate sediment with a calcite (plus aragonite) to dolomite ratio greater than 1 to 1. Includes lime-sediments.","after Hallsworth & Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/calcareous_carbonate_sedimentary_material","Calcareous carbonate sedimentary material","Carbonate sedimentary material of unspecified consolidation state with a calcite (plus aragonite) to dolomite ratio greater than 1 to 1. Includes lime-sediments, limestone and dolomitic limestone.","after Hallsworth & Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/calcareous_carbonate_sedimentary_rock","Calcareous carbonate sedimentary rock","Carbonate sedimentary rock with a calcite (plus aragonite) to dolomite ratio greater than 1 to 1. Includes limestone and dolomitic limestone.","SLTTs 2004, Hallsworth & Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_mud","Carbonate mud","Carbonate sediment composed of less than 25 percent clasts  that have a maximum diameter more than 2 mm, and the ratio of sand size to mud size clasts is less than one.","follow pattern used for clastic sand and mud categories, based on SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_mudstone","Carbonate mudstone","Mudstone that consists of greater than 50 percent carbonate minerals of any origin in the mud size fraction.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_ooze","Carbonate ooze","ooze that consists of more than 50 percent carbonate skeletal remains","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_rich_mud","Carbonate rich mud","Mud size sediment that contains between 10 and 50 percent carbonate minerals in any size fraction. Carbonate origin is not specified.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_rich_mudstone","Carbonate rich mudstone","Mudstone that contains between 10 and 50 percent carbonate minerals in the mud size fraction. Carbonate origin is not specified.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_sediment","Carbonate sediment","Sediment in which at least 50 percent of the primary and/or recrystallized constituents are composed of one (or more) of the carbonate minerals calcite, aragonite and dolomite, in particles of intrabasinal origin.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_sedimentary_material","Carbonate sedimentary material","Sedimentary material in which at least 50 percent of the primary and/or recrystallized constituents are composed of one (or more) of the carbonate minerals calcite, aragonite and dolomite, in particles of intrabasinal origin.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_sedimentary_rock","Carbonate sedimentary rock","Sedimentary rock in which at least 50 percent of the primary and/or recrystallized constituents are composed of one (or more) of the carbonate minerals calcite, aragonite, magnesite or dolomite.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonate_wackestone","Carbonate wackestone","Carbonate sedimentary rock with discernible mud supported depositional texture and containing greater than 10 percent allochems, and constituent particles are of intrabasinal origin. If particles are not intrabasinal, categorization as a mudstone or wackestone should be considered.","Dunham 1962"]
["http://resource.geosciml.org/classifier/cgi/lithology/carbonatite","Carbonatite","Igneous rock composed of more than 50 percent modal carbonate minerals.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/cataclasite_series","Cataclasite series","Fault-related rock that maintained primary cohesion during deformation, with matrix comprising greater than 10 percent of rock mass, matrix is fine-grained material formed through grain size reduction by fracture as opposed to crystal plastic process that operate in mylonitic rock.  Includes cataclasite, protocataclasite and ultracataclasite.","Sibson, 1977, Scholz, 1990, Snoke and Tullis, 1998, Barker, 1998 Appendix II, NADM SLTTm, 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/chalk","Chalk","A generally soft, white, very fine-grained, extremely pure, porous limestone. It forms under marine conditions from the gradual accumulation of skeletal elements from minute planktonic green algae (cocoliths), associated with varying proportions of larger microscopic fragments of bivalves, foraminifera and ostracods. It is common to find flint and chert nodules embedded in chalk.","http://en.wikipedia.org/wiki/Chalk, C.S. Harris, 2009, unpublished web pagehttp://www.geologyshop.co.uk/chalk.htm"]
["http://resource.geosciml.org/classifier/cgi/lithology/chemical_sedimentary_material","Chemical sedimentary material","Sedimentary material  that consists of at least 50 percent material produced by inorganic chemical processes within the basin of deposition. Includes inorganic siliceous, carbonate, evaporite, iron-rich, and phosphatic sediment classes.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/chlorite_actinolite_epidote_metamorphic_rock","Chlorite actinolite epidote metamorphic rock","Metamorphic rock characterized by 50 percent or more of combined chlorite, actinolite and epidote. Category for rocks generally named greenschist or greenstone.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/clastic_conglomerate","Conglomerate","Clastic sedimentary rock composed of at least 30 percent rounded to subangular fragments larger than 2 mm in diameter, typically contains finer grained material in interstices between larger fragments. If more than 15 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wackestone. If rock has unsorted or poorly sorted texture with a wide range of particle sizes, may also be categorized as diamictite.","Neuendorf et al. 2005, SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/clastic_mudstone","Mudstone","Clastic sedimentary rock consisting of less than 30 percent gravel-size (2 mm) particles and with a mud to sand ratio greater than 1.","Pettijohn et al. 1987 referenced in Hallsworth & Knox 1999."]
["http://resource.geosciml.org/classifier/cgi/lithology/clastic_sandstone","Sandstone","Clastic sedimentary rock in which less than 30 percent of particles are greater than 2 mm in diameter (gravel) and the sand to mud ratio is at least 1.","SLTTs 2004, Neuendorf et al. 2005, particle size from Wentworth grade scale"]
["http://resource.geosciml.org/classifier/cgi/lithology/clastic_sediment","Clastic sediment","Sediment in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.","SLTTs 2004, Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/clastic_sedimentary_material","Clastic sedimentary material","Sedimentary material of unspecified consolidation state in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.","SLTTs 2004, Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/clastic_sedimentary_rock","Clastic sedimentary rock","Sedimentary rock in which at least 50 percent of the constituent particles were derived from erosion, weathering, or mass-wasting of pre-existing earth materials, and transported to the place of deposition by mechanical agents such as water, wind, ice and gravity.","SLTTs 2004, Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/clay","Clay","Mud that consists of greater than 50 percent particles with grain size less than 0.004 mm","based on SLTTs 2004, Neuendorf et al. 2005, particle size from Wentworth grade scale"]
["http://resource.geosciml.org/classifier/cgi/lithology/claystone","Claystone","Mudstone that contains no detectable silt, inferred to consist virtually entirely of clay-size particles.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/coal","Coal","A consolidated organic sedimentary material having less than 75% moisture. This category includes low, medium, and high rank coals according to International Classification of In-Seam Coal (United Nations, 1998), thus including lignite. Sapropelic coal is not distinguished in this category from humic coals. Formed from the compaction or induration of variously altered plant remains similar to those of peaty deposits.","Economic Commission for Europe, Committee on Sustainable Energy- United Nations (ECE-UN), 1998, International Classification of in-Seam Coals: Energy 19, 41 pp."]
["http://resource.geosciml.org/classifier/cgi/lithology/cobble_gravel_size_sediment","Cobble gravel size sediment^^xsd:string","Sediment containing greater than 30 percent cobble-size particles (64-256 mm in diameter)^^xsd:string","Wentworth size scale^^xsd:string"]
["http://resource.geosciml.org/classifier/cgi/lithology/composite_genesis_material","Composite genesis material","Material of unspecified consolidation state formed by geological modification of pre-existing materials outside the realm of igneous and sedimentary processes. Includes rocks formed by impact metamorphism, standard dynamothermal metamorphism, brittle deformation, weathering, metasomatism and hydrothermal alteration (diagenesis is a sedimentary process in this context).","SLTTm 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/composite_genesis_rock","Composite genesis rock","Rock formed by geological modification of pre-existing rocks outside the realm of igneous and sedimentary processes. Includes rocks formed by impact metamorphism, standard dynamothermal metamorphism, brittle deformation, weathering, metasomatism and hydrothermal alteration (diagenesis is a sedimentary process in this context).","SLTTm 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/compound_material","Compound material","An Earth Material composed of an aggregation of particles of Earth Material, possibly including other Compound Materials. This is 'top' of lithology category hierarchy, and should be used to indicate 'any rock or unconsolidated material'.","NADM C1 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/crystalline_carbonate","Crystalline carbonate","Carbonate rock of indeterminate mineralogy in which diagenetic processes have obliterated any original depositional texture.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/dacite","Dacite","Fine grained or porphyritic crystalline rock that contains less than 90 percent mafic minerals,  between 20 and 60 percent quartz in the QAPF fraction, and has a plagioclase to total feldspar ratio greater than 0.65.  Includes rocks defined modally in QAPF fields 4 and 5 or chemically in TAS Field O3. Typcially composed of quartz and sodic plagioclase with minor amounts of biotite and/or hornblende and/or pyroxene, fine-grained equivalent of granodiorite and tonalite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/diamictite","Diamictite","Unsorted or poorly sorted, clastic sedimentary rock with a wide range of particle sizes including a muddy matrix.  Biogenic materials that have such texture are excluded. Distinguished from conglomerate, sandstone, mudstone based on polymodality and  lack of structures related to transport and deposition of sediment by moving air or water.  If more than 10 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wacke.","Fairbridge and Bourgeois 1978"]
["http://resource.geosciml.org/classifier/cgi/lithology/diamicton","Diamicton","Unsorted or poorly sorted, clastic sediment with a wide range of particle sizes, including a muddy matrix.  Biogenic materials that have such texture are excluded. Distinguished from conglomerate, sandstone, mudstone based on polymodality and  lack of structures related to transport and deposition of sediment by moving air or water. Assignment to an other size class can be used in conjunction to indicate the dominant grain size.","Fairbridge and Bourgeois 1978"]
["http://resource.geosciml.org/classifier/cgi/lithology/diorite","Diorite","Phaneritic crystalline rock consisting of intermediate plagioclase, commonly with hornblende and often with biotite or augite, colour index M less than 90,  sodic plagioclase (An0-An50), no feldspathoid, and between 0 and 5 percent quartz. Includes rocks defined modally in QAPF field 10 as diorite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/dioritic_rock","Dioritic rock","Phaneritic crystalline rock with M less than 90, consisting of intermediate plagioclase, commonly with hornblende and often with biotite or augite. A dioritoid with a plagioclase to total feldspar ratio (in the QAPF fraction) greater than 0.9.  Includes rocks defined modally in QAPF fields 10, 10' and 10*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/dioritoid","Dioritoid","Phaneritic crystalline igneous rock with M less than 90, consisting of intermediate plagioclase, commonly with hornblende and often with biotite or augite. Plagioclase to total feldspar ratio is greater that 0.65, and anorthite content of plagioclase is less than 50 percent. Less than 10 percent feldspathoid mineral and less than 20 percent quartz in the QAPF fraction.  Includes rocks defined modally in QAPF fields 9 and 10 (and their subdivisions).","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/doleritic_rock","Doleritic rock","Dark colored gabbroic (basaltic) or dioritic (andesitic) rock intermediate in grain size between basalt and gabbro and composed of plagioclase, pyroxene and opaque minerals, often with ophitic texture. Typically occurs as hypabyssal intrusions. Includes dolerite, microdiorite, diabase and microgabbro.","Neuendorf et al 2005, LeMaitre et al. 2002, Gillespie and Styles 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/dolomitic_or_magnesian_sedimentary_material","Dolomitic or magnesian sedimentary material","Carbonate sedimentary material of unspecified consolidation degree with a ratio of magnesium carbonate to calcite (plus aragonite) greater than 1 to 1. Includes dolomite sediment, dolostone, lime dolostone and magnesite-stone.","after SLTTs 2004hallsworth and Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/dolomitic_or_magnesian_sedimentary_rock","Dolomitic or magnesian sedimentary rock","Carbonate sedimentary rock with a ratio of magnesium carbonate to calcite (plus aragonite) greater than 1 to 1. Includes dolostone, lime dolostone and magnesite-stone.","after SLTTs 2004hallsworth and Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/dolomitic_sediment","Dolomitic sediment","Carbonate sediment with a ratio of magnesium carbonate to calcite (plus aragonite) greater than 1 to 1.","after SLTTs 2004hallsworth and Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/dolostone","Dolomite","Pure carbonate sedimentary rock with a ratio of magnesium carbonate to calcite (plus aragonite) greater than 1 to 1.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/duricrust","Duricrust","Rock forming a hard crust or layer at or near the Earth's surface at the time of formation, e.g. in the upper horizons of a soil, characterized by structures indicative of pedogenic origin.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/eclogite","Eclogite","Metamorphic rock composed of 75 percent or more (by volume) omphacite and garnet, both of which are present as major constituents, the amount of neither of them being higher than 75 percent (by volume), the presence of plagioclase precludes classification as an eclogite.","IUGS SCMR 2007 (http://www.bgs.ac.uk/SCMR/)"]
["http://resource.geosciml.org/classifier/cgi/lithology/evaporite","Evaporite","Nonclastic sedimentary rock composed of at least 50 percent non-carbonate salts, including chloride, sulfate or borate minerals, formed through precipitation of mineral salts from a saline solution (non-carbonate salt rock).","Jackson 1997, SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/exotic_alkaline_rock","Exotic alkaline rock","Kimberlite, lamproite, or lamprophyre. Generally are potassic, mafic or ultramafic rocks. Olivine (commonly serpentinized in kimberlite), and phlogopite are significant constituents.","based on LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/exotic_composition_igneous_rock","Exotic composition igneous rock","Rock with 'exotic' mineralogical, textural or field setting characteristics, typically dark colored, with abundant phenocrysts. Criteria include: presence of greater than 10 percent melilite or leucite, or presence of kalsilite, or greater than 50 percent carbonate minerals. Includes Carbonatite, Melilitic rock, Kalsilitic rocks, Kimberlite, Lamproite, Leucitic rock and Lamprophyres.","Gillespie and Styles 1999, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/exotic_evaporite","Exotic evaporite","Evaporite that is not 50 percent halite or 50 percent gypsum or anhydrite.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/fault_related_material","Fault-related material","Material formed as a result brittle faulting, composed of greater than 10 percent matrix, matrix is fine-grained material caused by tectonic grainsize reduction. Includes cohesive (cataclasite series) and non-cohesive (breccia-gouge series) material.","This vocabulary, SLTTm 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/fine_grained_igneous_rock","Fine grained igneous rock","Igneous rock in which the framework of the rock consists of crystals that are too small to determine mineralogy with the unaided eye, framework may include up to 50 percent glass. A significant percentage of the rock by volume may be phenocrysts. Includes rocks that are generally called volcanic rocks.","Gillespie and Styles 1999, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_alkali_feldspar_syenite","Foid bearing alkali feldspar syenite","Alkali feldspar syenitic rock that contains 0-10 percent feldspathoid mineral and no quartz in the QAPF fraction. QAPF field 6'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_alkali_feldspar_trachyte","Foid bearing alkali feldspar trachyte","Alkali feldspar trachytic rock that contains no quartz and between 0 and 10 percent feldspathoid mineral in the QAPF fraction. QAPF field 6'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_anorthosite","Foid bearing anorthosite","Anorthositic rock that contains between 0 and 10 percent feldspathoid mineral and no quartz in the QAPF fraction. QAPF field 10'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_diorite","Foid bearing diorite","Dioritic rock that contains between 0 and 10 percent feldspathoid minerals in the QAPF fraction. QAPF field 10'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_gabbro","Foid bearing gabbro","Gabbroic rock that contains 0-10 percent feldspathoid minerals and no quartz in the QAPF fraction. QAPF field 10'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_latite","Foid bearing latite","Latitic rock that contains no quartz and between 0 and 10 percent feldspathoid minerals in the QAPF fraction. QAPF field 8'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_monzodiorite","Foid bearing monzodiorite","Monzodioritic rock that contains between 0 and 10 percent feldspathoid mineral.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_monzogabbro","Foid bearing monzogabbro","Monzogabbroic rock that contains 0 to 10 percent feldspathoid mineral in the QAPF fraction. QAPF field 9'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_monzonite","Foid bearing monzonite","Monzonitic rock that contains 0-10 percent feldspathoid mineral and no quartz in the QAPF fraction. Includes rocks defined modally in QAPF Field 8'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_syenite","Foid bearing syenite","Syenitic rock that contains between 0 and 10 percent feldspathoid mineral and no quartz in the QAPF fraction. Defined modally in QAPF Field 7'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_bearing_trachyte","Foid bearing trachyte","Trachytic rock that contains between 0 and 10 percent feldspathoid in the QAPF fraction, and no quartz. QAPF field 7'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_diorite","Foid diorite","Foid dioritoid in which the plagioclase to total feldspar ratio is greater than 0.9.  Includes rocks defined modally in QAPF field 14.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_dioritoid","Foid dioritoid","Phaneritic crystalline igneous rock in which M is less than 90, the plagioclase to total feldspar ratio is greater than 0.5,  feldspathoid minerals form 10-60 percent of the QAPF fraction,  plagioclase has anorthite content less than 50 percent. These rocks typically contain large amounts of mafic minerals. Includes rocks defined modally in QAPF fields 13 and 14.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_gabbro","Foid gabbro","Foid gabbroid that has a plagioclase to total feldspar ratio greater than 0.9. Includes rocks defined modally in QAPF field 14.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_gabbroid","Foid gabbroid","Phaneritic crystalline igneous rock in which M is less than 90, the plagioclase to total feldspar ratio is greater than 0.5,  feldspathoids form 10-60 percent of the QAPF fraction, and plagioclase has anorthite content greater than 50 percent. These rocks typically contain large amounts of mafic minerals. Includes rocks defined modally in QAPF fields 13 and 14.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_monzodiorite","Foid monzodiorite","Foid dioritoid in which the plagioclase to total feldspar ratio is between 0.1 and 0.9.  Includes rocks defined modally in QAPF field 13.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_monzogabbro","Foid monzogabbro","Foid gabbroid that has a plagioclase to total feldspar ratio between 0.5 and 0.9. Includes rocks defined modally in QAPF field 13.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_monzosyenite","Foid monzosyenite","Foid syenitoid rock that has a plagioclase to total feldspar ratio of between 0.1 and 0.5.  Includes rocks defined modally in QAPF Field 12.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_syenite","Foid syenite","Foid syenitoid that has a plagioclase to total feldspar ratio of less than 0.1. Includes rocks defined modally in QAPF field 11.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foid_syenitoid","Foid syenitoid","Phaneritic crystalline igneous rock with M less than 90, contains between 10 and 60 percent feldspathoid mineral in the QAPF fraction, and has a plagioclase to total feldspar ratio less than 0.5. Includes QAPF fields 11 and 12.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foidite","Foidite","Foiditoid that contains greater than 90 percent feldspathoid minerals in the QAPF fraction.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foiditoid","Foiditoid","Fine grained crystalline rock containing less than 90 percent mafic minerals and more than 60 percent feldspathoid minerals in the QAPF fraction. Includes rocks defined modally in QAPF field 15 or chemically in TAS field F.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foidolite","Foidolite","Phaneritic crystalline rock containing more than 60 percent feldspathoid minerals in the QAPF fraction. Includes rocks defined modally in QAPF field 15","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/foliated_metamorphic_rock","Foliated metamorphic rock","Metamorphic rock in which 10 percent or more of the contained mineral grains are elements in a planar or linear fabric. Cataclastic or glassy character precludes classification with this concept.","based on NADM SLTT metamorphic"]
["http://resource.geosciml.org/classifier/cgi/lithology/fragmental_igneous_material","Fragmental igneous material","igneous_material of unspecified consolidation state in which greater than 75 percent of the rock consists of fragments produced as a result of igneous rock-forming process.","CGI concept definition task group"]
["http://resource.geosciml.org/classifier/cgi/lithology/fragmental_igneous_rock","Fragmental igneous rock","Igneous rock in which greater than 75 percent of the rock consists of fragments produced as a result of igneous rock-forming process. Includes pyroclastic rocks, autobreccia associated with lava flows and intrusive breccias. Excludes deposits reworked by epiclastic processes (see Tuffite)","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/framestone","Framestone","Carbonate reef rock consisting of a rigid framework of colonies, shells or skeletons, with internal cavities filled with fine sediment, usually created through the activities of colonial organisms.","Hallsworth & Knox 1999, SLTTs 2004, Table 15-3-1"]
["http://resource.geosciml.org/classifier/cgi/lithology/gabbro","Gabbro","Gabbroic rock that contains between 0 and 5 percent quartz and no feldspathoid mineral in the QAPF fraction.  Includes rocks defined modally in QAPF Field 10 as gabbro.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/gabbroic_rock","Gabbroic rock","Gabbroid that has a plagioclase to total feldspar ratio greater than 0.9 in the QAPF fraction.  Includes QAPF fields 10*, 10, and 10'. This category includes the various categories defined in LeMaitre et al. (2002) based on the mafic mineralogy, but apparently not subdivided based on the quartz/feldspathoid content.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/gabbroid","Gabbroid","Phaneritic crystalline igneous rock that contains less than 90 percent mafic minerals, and up to 20 percent quartz or up to 10 percent feldspathoid in the QAPF fraction. The ratio of plagioclase to total feldspar is greater than 0.65, and anorthite content of the plagioclase is greater than 50 percent. Includes rocks defined modally in QAPF fields 9 and 10 and their subdivisions.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/generic_conglomerate","Generic conglomerate","Sedimentary rock composed of at least 30 percent rounded to subangular fragments larger than 2 mm in diameter, typically contains finer grained material in interstices between larger fragments. If more than 15 percent of the fine grained matrix is of indeterminant clastic or diagenetic origin and the fabric is matrix supported, may also be categorized as wackestone. If rock has unsorted or poorly sorted texture with a wide range of particle sizes, may also be categorized as diamictite.","Neuendorf et al. 2005, SLTTs 2004, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/generic_mudstone","Generic mudstone","Sedimentary rock consisting of less than 30 percent gravel-size (2 mm) particles and with a mud to sand ratio greater than 1. Clasts may be of any composition or origin.","Pettijohn et al. 1987 referenced in Hallsworth & Knox 1999, extrapolated from Folk, 1954, Figure 1a, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/generic_sandstone","Generic sandstone","Sedimentary rock in which less than 30 percent of particles are greater than 2 mm in diameter (gravel) and the sand to mud ratio is at least 1.","SLTTs 2004, Neuendorf et al. 2005, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/glass_rich_igneous_rock","Glass rich igneous rock","Igneous rock that contains greater than 50 percent massive glass.","This vocabulary, based on Gillespie and Styles 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/glassy_igneous_rock","Glassy igneous rock","Igneous rock that consists of greater than 80 percent massive glass.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/glaucophane_lawsonite_epidote_metamorphic_rock","Glaucophane lawsonite epidote metamorphic rock","A metamorphic rock of roughly basaltic composition, defined by the presence of glaucophane with lawsonite or epidote. Other minerals that may be present include jadeite, albite, chlorite, garnet, and muscovite (phengitic white mica). Typically fine-grained, dark colored. Category for rocks commonly referred to as blueschist.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/gneiss","Gneiss","Foliated metamorphic rock with bands or lenticles rich in granular minerals alternating with bands or lenticles rich in minerals with a flaky or elongate prismatic habit. Mylonitic foliation or well developed, continuous schistosity (greater than 50 percent of the rock consists of grains participate in a planar or linear fabric) precludes classification with this concept.","Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/grainstone","Grainstone","Carbonate sedimentary rock with recognizable depositional fabric that is grain-supported, and constituent particles are of intrabasinal origin, contains little or no mud matrix. Distinction from sandstone is based on interpretation of intrabasinal origin of clasts and grain-supported fabric, but grainstone definition does not include a grain size criteria.","Dunham 1962"]
["http://resource.geosciml.org/classifier/cgi/lithology/granite","Granite","Phaneritic crystalline rock consisting of quartz, alkali feldspar and plagioclase (typically sodic) in variable amounts, usually with biotite and/or hornblende. Includes rocks defined modally in QAPF Field 3.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/granitoid","Granitoid","Phaneritic crystalline igneous rock consisting of quartz, alkali feldspar and/or plagioclase. Includes rocks defined modally in QAPF fields 2, 3, 4 and 5 as alkali feldspar granite, granite, granodiorite or tonalite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/granodiorite","Granodiorite","Phaneritic crystalline rock consisting essentially of quartz, sodic plagioclase and lesser amounts of alkali feldspar with minor hornblende and biotite. Includes rocks defined modally in QAPF field 4.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/granofels","Granofels","Metamorphic rock with granoblastic fabric and very little or no foliation (less than 10 percent of the mineral grains in the rock are elements in a planar or linear fabric). Grainsize not specified.","SLTTm 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/granulite","Granulite","Metamorphic rock of high metamorphic grade in which Fe-Mg silicate minerals are dominantly hydroxl-free, feldspar must be present, and muscovite is absent, rock contains less than 90 percent mafic minerals,  less than 75 percent calcite and/or dolomite, less than 75 percent quartz, less than 50 percent iron-bearing minerals (hematite, magnetite, limonite-group, siderite, iron-sulfides), and less than 50 percent calc-silicate minerals.","Fettes and Desmons (2007).  See also  Wimmenauer (1985), Winkler (1979) (D.R. Bowes (1989), The Encyclopedia of Igneous and Metamorphic Petrology, Van Nostrand Reinhold ISBN: 0-442-20623-2 wikipediahttp://en.wikipedia.org/wiki/Granulite accessed 5/30/09"]
["http://resource.geosciml.org/classifier/cgi/lithology/gravel","Gravel","Clastic sediment containing greater than 30 percent gravel-size particles (greater than 2.0 mm diameter). Gravel in which more than half of the particles are of epiclastic origin","definition of gravel from SLTTs 2004, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/gravel_size_sediment","Gravel size sediment","Sediment containing greater than 30 percent gravel-size particles (greater than 2.0 mm diameter). Composition or gensis of clasts not specified.","SLTTs 2004, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/high_magnesium_fine_grained_igneous_rocks","High magnesium fine grained igneous rock","fine-grained igneous rock that contains unusually high concentration of MgO. For rocks that contain greater than 52 percent silica, MgO must be greater than 8 percent. For rocks containing less than 52 percent silica, MgO must be greater than 12 percent.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/hornblendite","Hornblendite","Ultramafic rock that consists of greater than 40 percent hornblende plus pyroxene and has a hornblende to pyroxene ratio greater than 1. Includes olivine hornblendite, olivine-pyroxene hornblendite, pyroxene hornblendite, and hornblendite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/hornfels","Hornfels","Granofels formed by contact metamorphism, composed of a mosaic of equidimensional grains in a characteristically granoblastic or decussate matrix, porphyroblasts or relict phenocrysts may be present. Typically fine grained.","IUGS SCMR 2007 (http://www.bgs.ac.uk/SCMR/)"]
["http://resource.geosciml.org/classifier/cgi/lithology/hybrid_sediment","Hybrid sediment","Sediment that does not fit any of the other sediment composition/genesis categories. Sediment consisting of three or more components which form more than 5 percent but less than 50 precent  of the material.","Hallsworth and Knox, 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/hybrid_sedimentary_rock","Hybrid sedimentary rock","Sedimentary rock that does not fit any of the other  composition/genesis categories. Sedimentary rock consisting of three or more components which form more than 5 percent but less than 50 precent  of the material.","Hallsworth and Knox, 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/igneous_material","Igneous material","Earth material formed as a result of igneous processes, eg. intrusion and cooling of magma in the crust, volcanic eruption.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/igneous_rock","Igneous rock","rock formed as a result of igneous processes, for example intrusion and cooling of magma in the crust, or volcanic eruption.","Neuendorf et al 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/impact_generated_material","Impact generated material","Material that contains features indicative of shock metamorphism, such as microscopic planar deformation features within grains or shatter cones, interpreted to be the result of extraterrestrial bolide impact. Includes breccias and melt rocks.","Stöffler and Grieve 2007, Jackson 1997"]
["http://resource.geosciml.org/classifier/cgi/lithology/impure_calcareous_carbonate_sediment","Impure calcareous carbonate sediment","Carbonate sediment in which between 50 and 90 percent of the constituents are composed of one (or more) of the carbonate minerals in particles of intrabasinal origin, and a calcite (plus aragonite) to dolomite ratio greater than 1 to 1.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/impure_carbonate_sediment","Impure carbonate sediment","Carbonate sediment in which between 50 and 90 percent of the constituents are composed of one (or more) of the carbonate minerals in particles of intrabasinal origin.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/impure_carbonate_sedimentary_rock","Impure carbonate sedimentary rock","Sedimentary rock in which between 50 and 90 percent of the primary and/or recrystallized constituents are composed of carbonate minerals.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/impure_dolomitic_sediment","Impure dolomitic sediment","Carbonate sediment in which between 50 and 90 percent of the constituents are composed of one (or more) of the carbonate minerals in particles of intrabasinal origin, and the ratio of magnesium carbonate to calcite (plus aragonite) greater than 1 to 1.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/impure_dolostone","Impure dolomite","Impure carbonate sedimentary rock with a ratio of magnesium carbonate to calcite (plus aragonite) greater than 1 to 1.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/impure_limestone","Impure limestone","Impure carbonate sedimentary rock with a calcite (plus aragonite) to dolomite ratio greater than 1 to 1.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/intermediate_composition_igneous_material","Intermediate composition igneous material","Igneous material with between 52 and 63 percent SiO2.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/intermediate_composition_igneous_rock","Intermediate composition igneous rock","Igneous rock with between 52 and 63 percent SiO2.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/iron_rich_sediment","Iron rich sediment","Sediment that consists of at least 50 percent iron-bearing minerals (hematite, magnetite, limonite-group, siderite, iron-sulfides), as determined by hand-lens or petrographic analysis. Corresponds to a rock typically containing 15 percent iron by weight.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/iron_rich_sedimentary_material","Iron rich sedimentary material","Sedimentary material of unspecified consolidation state that consists of at least 50 percent iron-bearing minerals (hematite, magnetite, limonite-group, siderite, iron-sulfides), as determined by hand-lens or petrographic analysis. Corresponds to a rock typically containing 15 percent iron by weight.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/iron_rich_sedimentary_rock","Iron rich sedimentary rock","Sedimentary rock that consists of at least 50 percent iron-bearing minerals (hematite, magnetite, limonite-group, siderite, iron-sulfides), as determined by hand-lens or petrographic analysis. Corresponds to a rock typically containing 15 percent iron by weight.","Hallsworth and Knox 1999, SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/kalsilitic_and_melilitic_rock","Kalsilitic and melilitic rocks","Igneous rock containing greater than 10 percent melilite or kalsilite. Typically undersaturated, ultrapotassic (kalsilitic rocks) or calcium-rich (melilitic rocks) mafic or ultramafic rocks.","based on LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/komatiitic_rock","Komatiitic rock","Ultramafic, magnesium-rich volcanic rock, typically with spinifex texture of intergrown skeletal and bladed olivine and pyroxene crystals set in abundant glass. Includes komatiite and meimechite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/latite","Latite","Latitic rock that contains between 0 and 5 percent quartz and no feldspathoid in the QAPF fraction. QAPF field 8.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/latitic_rock","Latitic rock","Trachytoid that has a plagioclase to total feldspar ratio between 0.35 and 0.65. QAPF fields 8, 8' and 8*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/lignite","Lignite","Coal that has a gross calorific value less than 24 MJ/kg (determined in conformance with ISO 1928), and vitrinite mean random reflectance less than 0.6% (determined in conformance with ISO 7404-5). Gross calorific value is recalculated to a moist, ash free basis using bed moisture (determined according to ISO 1015 or ISO 5068). Includes all low-rank coals, including sub-bitiminous coal. A consolidated, dull, soft brown to black coal having many readily discernible plant fragments set in a finer grained organic matrix. Tends to crack and fall apart on drying. Operationally sub-bituminous and bitiminous coal are qualitatively distinguished based on brown streak for sub-bitiminous coal and black streak for bituminous coal.","Economic Commission for Europe, Committee on Sustainable Energy- United Nations (ECE-UN), 1998, International Classification of in-Seam Coals: Energy 19, 41 pp."]
["http://resource.geosciml.org/classifier/cgi/lithology/limestone","Limestone","Pure carbonate sedimentary rock with a calcite (plus aragonite) to dolomite ratio greater than 1 to 1.  Includes limestone and dolomitic limestone.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/marble","Marble","Metamorphic rock consisting of greater than 75 percent fine- to coarse-grained recrystallized calcite and/or dolomite, usually with a granoblastic, saccharoidal texture.","IUGS SCMR 2007 (http://www.bgs.ac.uk/SCMR/), SLTTm1.0 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/material_formed_in_surficial_environment","Material formed in surficial environment","Material that is the product of weathering processes operating on pre-existing rocks or deposits, analogous to hydrothermal or metasomatic rocks, but formed at ambient Earth surface temperature and pressure.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/metamorphic_rock","Metamorphic rock","Rock formed by solid-state mineralogical, chemical and/or structural changes to a pre-existing rock, in response to marked changes in temperature, pressure, shearing stress and chemical environment.","Jackson 1997"]
["http://resource.geosciml.org/classifier/cgi/lithology/metasomatic_rock","Metasomatic rock","Rock that has fabric and composition indicating open-system mineralogical and chemical changes in response to interaction with a fluid phase, typically water rich.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/mica_schist","Mica schist","A schist that consists of more than 50 percent mica minerals, typically muscovite or biotite. Special type included to distinguish this common variety of schist.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/migmatite","Migmatite","Silicate metamorphic rock that is pervasively heterogeneous on a decimeter to meter scale that typically consists of darker and lighter parts, the darker parts usually exhibit features of metamorphic rocks whereas the lighter parts are of igneous-looking appearance.","Fette and Desmons (2007) (http://www.bgs.ac.uk/SCMR/)"]
["http://resource.geosciml.org/classifier/cgi/lithology/monzodiorite","Monzodiorite","Phaneritic crystalline igneous rock consisting of sodic plagioclase (An0 to An50), alkali feldsparhornblende and biotite, with or without pyroxene, and  0 to 5 percent quartz. Includes rocks defined modally in QAPF field 9.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/monzodioritic_rock","Monzodioritic rock","Phaneritic crystalline igneous rock consisting of sodic plagioclase (An0 to An50), alkali feldsparhornblende and biotite, with or without pyroxene, and 0 to 10 percent feldspathoid or 0 to 20 percent quartz in the QAPF fraction. Plagioclase to total feldspar ratio in the QAPF fraction is between 0.65 and 0.9.  Includes rocks defined modally in QAPF field 9, 9' and 9* as monzodiorite, foid-beaing  monzodiorite, and quartz monzodiorite.","This vocabulary, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/monzogabbro","Monzogabbro","Monzogabbroic rock that contains between 0 an 5 percent quartz and no feldspathoid mineral in the QAPF fraction.  Includes rocks defined modally in QAPF field 9 .","LeMaitre et al. 2002, This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/monzogabbroic_rock","Monzogabbroic rock","Gabbroid with a plagioclase to total feldspar ratio between 0.65 and 0.9. QAPF field 9, 9 prime and 9 asterisk","LeMaitre et al. 2002, This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/monzogranite","Monzogranite","Granite that has a plagiolcase to total feldspar ratio between 0.35 and 0.65. QAPF field 3b.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/monzonite","Monzonite","Monzonitic rock that contains 0-5 percent quartz and no feldspathoid mineral in the QAPF fraction. Includes rocks defined modally in QAPF Field 8.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/monzonitic_rock","Monzonitic rock","Syenitoid with a plagioclase to total feldspar ratio between 0.35 and 0.65. Includes rocks in QAPF fields 8, 8*, and 8'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/mud","Mud","Clastic sediment consisting of less than 30 percent gravel-size (2 mm) particles and with a mud-size to sand-size particle ratio greater than 1. More than half of the particles are of epiclastic origin.","definition of mud from SLTTs 2004 muddy sediment, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/mud_size_sediment","Mud size sediment","Sediment consisting of less than 30 percent gravel-size (2 mm) particles and with a mud-size to sand-size particle ratio greater than 1. Clasts may be of any composition or origin.","based on SLTTs 2004, Neuendorf et al. 2005, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/mylonitic_rock","Mylonitic rock","Metamorphic rock characterised by a foliation resulting from tectonic grain size reduction, in which more than 10 percent of the rock volume has undergone grain size reduction. Includes protomylonite, mylonite, ultramylonite, and blastomylonite.","Marshak & Mitra 1988"]
["http://resource.geosciml.org/classifier/cgi/lithology/natural_unconsolidated_material","Natural unconsolidated material","Unconsolidated material known to have natural, ie. not human-made, origin.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/non_clastic_siliceous_sediment","Non-clastic siliceous sediment","Sediment that consists of at least 50 percent silicate mineral material, deposited directly by chemical or biological processes at the depositional surface, or in particles formed by chemical or biological processes within the basin of deposition.","NGMDB 2008, Hallsworth and Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/non_clastic_siliceous_sedimentary_material","Non-clastic siliceous sedimentary material","Sedimentary material that consists of at least 50 percent silicate mineral material, deposited directly by chemical or biological processes at the depositional surface, or in particles formed by chemical or biological processes within the basin of deposition.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/non_clastic_siliceous_sedimentary_rock","Non-clastic siliceous sedimentary rock","Sedimentary rock that consists of at least 50 percent silicate mineral material, deposited directly by chemical or biological processes at the depositional surface, or in particles formed by chemical or biological processes within the basin of deposition.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/ooze","Ooze","Biogenic sediment consisting of less than 1 percent gravel-size (greater than or equal to 2 mm) particles, with a sand to mud ratio less than 1 to 9, and less than 50 percent carbonate minerals.","based on Bates and Jackson 1987 & Hallsworth & Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/organic_bearing_mudstone","Organic bearing mudstone","Mudstone that contains a significant amount of organic carbon, typically kerogen. Commonly finely laminated, brown or black in color.","Neuendorf et al. 2005, http://en.wikipedia.org/wiki/Oil_shale"]
["http://resource.geosciml.org/classifier/cgi/lithology/organic_rich_sediment","Organic rich sediment","Sediment with color, composition, texture and apparent density indicating greater than 50 percent organic content by weight on a moisture-free basis.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/organic_rich_sedimentary_material","Organic rich sedimentary material","Sedimentary material in which 50 percent or more of the primary sedimentary material is organic carbon.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/organic_rich_sedimentary_rock","Organic rich sedimentary rock","Sedimentary rock with color, composition, texture and apparent density indicating greater than 50 percent organic content by weight on a moisture-free basis.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/orthogneiss","Orthogneiss","A gneiss with mineralogy and texture indicating derivation from a phaneritic igneous rock protolith.  Typically consists of abundant feldspar, with quartz, and variable hornblende, biotite, and muscovite, with a relatively homogeneous character.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/packstone","Packstone","Carbonate sedimentary rock with discernible grain supported depositional texture, containing greater than 10 percent grains, and constituent particles are of intrabasinal origin, intergranular spaces are filled by matrix.","Hallsworth & Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/paragneiss","Paragneiss","A gneiss with mineralogy and texture indicating derivation from a sedimentary rock protolith. Typically consists of abundant quartz, mica, or calcsilicate minerals, aluminosilicate minerals or garnet commonly present. Composition of rock tends to be more variable on a decimetric scale that in orthogneiss.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/peat","Peat","Unconsolidated organic-rich sediment composed of at least 50 percent semi-carbonised plant remains, individual remains commonly seen with unaided eye, yellowish brown to brownish black, generally fibrous texture, can be plastic or friable. In its natural state it can be readily cut and has a very high moisture content, generally greater than 90 percent. Liptinite to Inertinite ratio is less than one (Economic Commission for Europe, Committee on Sustainable Energy- United Nations (ECE-UN), 1998, International Classification of in-Seam Coals: Energy 19, 41 pp.)","Hallsworth & Knox 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/pebble_gravel_size_sediment","Pebble gravel size sediment","Sediment containing greater than 30 percent pebble-size particles (2.0 -64 mm in diameter)^^xsd:string","Wentworth size scale^^xsd:string"]
["http://resource.geosciml.org/classifier/cgi/lithology/pegmatite","Pegmatite","Exceptionally coarse grained crystalline rock with interlocking crystals, most grains are 1cm or more diameter, composition is generally that of granite, but the term may refer to the coarse grained facies of any type of igneous rock,usually found as irregular dikes, lenses, or veins associated with plutons or batholiths.","Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/peridotite","Peridotite","Ultramafic rock consisting of more than 40 percent (by volume) olivine with pyroxene and/or amphibole and little or no feldspar. Commonly altered to serpentinite. Includes rocks defined modally in the ultramafic rock classification as duniteharzburgite, lherzolite, wehrlite, olivinite, pyroxene peridotite, pyroxene hornblende peridotite or hornblende peridotite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/phaneritic_igneous_rock","Phaneritic igneous rock","Igneous rock in which the framework of the rock consists of individual crystals that can be discerned with the unaided eye. Bounding grain size is on the order of 32 to 100 microns. Igneous rocks with 'exotic' composition are excluded from this concept.","Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/phonolilte","Phonolite","Phonolitoid in which the plagioclase to total feldspar ratio is less than 0.1. Rock consists of alkali feldspar, feldspathoid minerals, and mafic minerals.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/phonolitic_basanite","Phonolitic basanite","Tephritoid that has a plagioclase to total feldspar ratio between 0.5 and  0.9, and contains more than 10 percent normative (CIPW) olivine.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/phonolitic_foidite","Phonolitic foidite","Foiditoid that contains less than 90 percent feldspathoid minerals in the QAPF fraction, and has a  plagioclase to total feldspar ratio that is less than 0.5","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/phonolitic_tephrite","Phonolitic tephrite","Tephritoid that has a plagioclase to total feldspar ratio between 0.5 and 0.9, and contains less than 10 percent normative (CIPW) olivine.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/phonolitoid","Phonolitoid","Fine grained igneous rock than contains less than 90 percent mafic minerals, between 10 and 60 percent feldspathoid mineral in the QAPF fraction and has a plagioclase to total feldspar ratio less than 0.5. Includes rocks defined modally in QAPF fields 11 and 12, and TAS field Ph.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/phosphate_rich_sediment","Phosphate rich sediment","Sediment in which at least 50 percent of the primary and/or recrystallized constituents are phosphate minerals.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/phosphate_rich_sedimentary_material","Phosphate rich sedimentary material","Sedimentary material in which at least 50 percent of the primary and/or recrystallized constituents are phosphate minerals.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/phosphorite","Phosphorite","Sedimentary rock in which at least 50 percent of the primary or recrystallized constituents are phosphate minerals. Most commonly occurs as a bedded primary or reworked secondary marine rock, composed of microcrystalline carbonate fluorapatite in the form of lamina, pellets, oolites and nodules, and skeletal, shell and bone fragments.","Hallsworth&Knox 1999, Jackson 1997"]
["http://resource.geosciml.org/classifier/cgi/lithology/phyllite","Phyllite","Rock with a well developed, continuous schistosity, an average grain size between 0.1 and 0.5 millimeters, and a silvery sheen on cleavage surfaces. Individual phyllosilicate grains are barely visible with the unaided eye.","IUGS SCMR 2007 (http://www.bgs.ac.uk/SCMR/)"]
["http://resource.geosciml.org/classifier/cgi/lithology/phyllonite","Phyllonite","Mylonitic rock composed largely of fine-grained mica that imparts a sheen to foliation surfaces, may have flaser lamination, isoclinal folding, and deformed veins, which indicate significant shearing. Macroscopically resembles phyllite, but formed by mechanical degradation of initially coarser rock.","NADM metamorphic rock vocabulary SLTTm1.0, Marshak & Mitra 1988"]
["http://resource.geosciml.org/classifier/cgi/lithology/porphyry","Porphyry","Igneous rock that contains conspicuous phenocrysts in a finer grained groundmass, groundmass itself may be phaneritic or fine-grained.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/pure_calcareous_carbonate_sediment","Pure calcareous carbonate sediment","Carbonate sediment in which greater than 90 percent of the  constituents are composed of one (or more) of the carbonate minerals in particles of intrabasinal origin, and a calcite (plus aragonite) to dolomite ratio greater than 1 to 1.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/pure_carbonate_mudstone","Pure carbonate mudstone","Mudstone that consists of greater than 90 percent carbonate minerals of intrabasinal orign in the mud fraction, and contains less than 10 percent allochems.  The original depositional texture is preserved and fabric is matrix supported. Carbonate mudstone of Dunham (1962)","Dunham 1962"]
["http://resource.geosciml.org/classifier/cgi/lithology/pure_carbonate_sediment","Pure carbonate sediment","Carbonate sediment in which greater than 90 percent of the  constituents are composed of one (or more) of the carbonate minerals in particles of intrabasinal origin.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/pure_carbonate_sedimentary_rock","Pure carbonate sedimentary rock","Sedimentary rock in which greater than 90 percent of the primary and/or recrystallized constituents are carbonate minerals.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/pure_dolomitic_sediment","Pure dolomitic sediment","Carbonate sediment in which greater than 90 percent of the  constituents are composed of one (or more) of the carbonate minerals in particles of intrabasinal origin, and a ratio of magnesium carbonate to calcite (plus aragonite) greater than 1 to 1.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/pyroclastic_material","Pyroclastic material","Fragmental igneous material that consists of more than 75 percent of particles formed by disruption as a direct result of volcanic action.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/pyroclastic_rock","Pyroclastic rock","Fragmental igneous rock that consists of greater than 75 percent fragments produced as a direct result of eruption or extrusion of magma from within the earth onto its surface. Includes autobreccia associated with lava flows and excludes deposits reworked by epiclastic processes.","based on LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/pyroxenite","Pyroxenite","Ultramafic phaneritic igneous rock composed almost entirely of one or more pyroxenes and occasionally biotitehornblende and olivine. Includes rocks defined modally in the ultramafic rock classification as olivine pyroxenite, olivine-hornblende pyroxenite, pyroxenite, orthopyroxenite, clinopyroxenite and websterite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_alkali_feldspar_syenite","Quartz alkali feldspar syenite","Alkali feldspar syenitic rock that contains 5 to 20 percent quartz and no feldspathoid in the QAPF fraction. QAPF field 6*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_alkali_feldspar_trachyte","Quartz alkali feldspar trachyte","Alkali feldspar trachytic rock that contains and between 5 and 20 percent quartz  mineral in the QAPF fraction. QAPF field 6*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_anorthosite","Quartz anorthosite","Anorthositic rock that contains between 5 and 20 percent quartz in the QAPF fraction. QAPF field 10*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_diorite","Quartz diorite","Dioritic rock that contains between 5 to 20 percent quartz in the QAPF fraction. QAPF field 10*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_gabbro","Quartz gabbro","Gabbroic rock that contains between 5 and 20 percent quartz in the QAPF fraction. QAPF field 10*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_latite","Quartz latite","Latitic rock that contains between 5 and 20 percent quartz in the QAPF fraction. QAPF field 8*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_monzodiorite","Quartz monzodiorite","Monzodioritic rock that contains between 5 and 20 percent quartz.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_monzogabbro","Quartz monzogabbro","Monzogabbroic rock that contains between 5 and 20 percent quartz in the QAPF fraction. QAPF field 9*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_monzonite","Quartz monzonite","Monzonitic rock that contains 5-20 percent quartz iin the QAPF fraction. Includes rocks defined modally in QAPF Field 8*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_rich_igneous_rock","Quartz rich igneous rock","Phaneritic crystalline igneous rock that contains less than 90 percent mafic minerals and contains greater than 60 percent quartz in the QAPF fraction.","Gillespie and Styles 1999, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_syenite","Quartz syenite","Syenitic rock that contains between 5 and 20 percent quartz in the QAPF fraction. Defined modally in QAPF Field 7*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartz_trachyte","Quartz trachyte","Trachytic rock that contains between 5 and 20 percent quartz in the QAPF fraction. QAPF field 7*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/quartzite","Quartzite","Metamorphic rock consisting of greater than or equal to 75 percent quartz, typically granoblastic texture.","after Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/residual_material","Residual material","Material of composite origin resulting from weathering processes at the Earth’s surface, with genesis dominated by removal of chemical constituents by aqueous leaching. Miinor clastic, chemical, or organic input may also contribute. Consolidation state is not inherent in definition, but typically material is unconsolidated or weakly consolidated.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/rhyolite","Rhyolite","rhyolitoid in which the ratio of plagioclase to total feldspar is between 0.1 and 0.65.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/rhyolitoid","Rhyolitoid","fine_grained_igneous_rock consisting of quartz and alkali feldspar, with minor plagioclase and biotite, in a microcrystalline, cryptocrystalline or glassy groundmass. Flow texture is common. Includes rocks defined modally in QAPF fields 2 and 3 or chemically in TAS Field R as rhyolite. QAPF normative definition is based on modal mineralogy thus: less than 90 percent mafic minerals, between 20 and 60 percent quartz in the QAPF fraction, and ratio of plagioclse to total feldspar is less than 0.65.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/rock","Rock","Consolidated aggregate of one or more EarthMaterials, or a body of undifferentiated mineral matter, or of solid organic material. Includes mineral aggregates such as granite, shale, marble, glassy matter such as obsidian, and organic material such a coal. Excludes unconsolidated materials.","Jackson, 1997, NADM C1 2004, Neuendorf et al 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/rock_gypsum_or_anhydrite","Gypsum or anhydrite","Evaporite composed of at least 50 percent gypsum or anhydrite.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/rock_salt","Rock salt","Evaporite composed of at least 50 percent halite.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/sand","Sand","Clastic sediment in which less than 30 percent of particles are gravel (greater than 2 mm in diameter) and the sand to mud ratio is at least 1. More than half of the particles are of epiclastic origin.","definition of sand from SLTTs 2004 sandy sediment, particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/sand_size_sediment","Sand size sediment","Sediment in which less than 30 percent of particles are gravel (greater than 2 mm in diameter) and the sand to mud ratio is at least 1. Composition or genesis of clasts not specified.","Neuendorf et al. 2005 particle sizes defined from Krumbein phi scale (W C Krumbein & L L Sloss, Stratigraphy and Sedimentation, 2nd edition, Freeman, San Francisco, 1963, Krumbein and Pettijohn, 1938, Manual of Sedimentary Petrography: New York, Appleton Century Co., Inc.)"]
["http://resource.geosciml.org/classifier/cgi/lithology/sapropel","Sapropel","Jelly like organic rich sediment composed of plant remains, usually algal. Liptinite to Inertinite ratio is greater than one (Economic Commission for Europe, Committee on Sustainable Energy- United Nations (ECE-UN), 1998, International Classification of in-Seam Coals: Energy 19, 41 pp.)","Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/schist","Schist","Foliated phaneritic metamorphic rock with well developed, continuous schistosity, meaning that greater than 50 percent of the rock by volume is mineral grains with a thin tabular, lamellar, or acicular prismatic crystallographic habit that are oriented in a continuous planar or linear fabric.","SLTTm 2004, Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/sediment","Sediment","Unconsolidated material consisting of an aggregation of particles transported or deposited by air, water or ice, or that accumulated by other natural agents, such as chemical precipitation, and that forms in layers on the Earth's surface. Includes epiclastic deposits.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/sedimentary_material","Sedimentary material","Material formed by accumulation of solid fragmental material deposited by air, water or ice, or material that accumulated by other natural agents such as chemical precipitation from solution or secretion by organisms. Includes both sediment and sedimentary rock. Includes epiclastic deposits.  All stated composition criteria are based on the mineral/ compound material (GeoSciML term)/particulate fraction of the material, irrespective of porosity or the pore-fluid. No distinctions are made based on porosity or pore fluid composition (except organic rich sediment in which liquid hydrocarbon content may be considered).","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/sedimentary_rock","Sedimentary rock","Rock formed by accumulation and cementation of solid fragmental material deposited by air, water or ice, or as a result of other natural agents, such as precipitation from solution, the accumulation of organic material, or from biogenic processes, including secretion by organisms. Includes epiclastic deposits.","SLTTs 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/serpentinite","Serpentinite","Rock consisting of more than 75 percent serpentine-group minerals, eg. antigorite, chrysotile or lizardite, accessory chlorite, talc and magnetite may be present, derived from hydration of ferromagnesian silicate minerals such as olivine and pyroxene.","Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/shale","Shale","Laminated mudstone that will part or break along thin, closely spaced layers parallel to stratification.","NADM SLTT sedimentary, 2004"]
["http://resource.geosciml.org/classifier/cgi/lithology/silicate_mud","Silicate mud","Mud size sediment that consists of less than 50 percent carbonate minerals.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/silicate_mudstone","Silicate mudstone","Mudstone that contains less than 10 percent carbonate minerals.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/siliceous_ooze","Siliceous ooze","ooze that consists of more than 50 percent siliceous skeletal remains","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/silt","Silt","Mud that consists of greater than 50 percent silt-size grains.","based on SLTTs 2004, Neuendorf et al. 2005, particle size from Wentworth grade scale"]
["http://resource.geosciml.org/classifier/cgi/lithology/siltstone","Siltstone","Mudstone that contains detectable silt. (see comments)","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/skarn","Skarn","Metasomatic rock consisting mainly of Ca-, Mg-, Fe-, or Mn-silicate minerals, which are free from or poor in water. Typically formed at the contact between a silicate rock or magma and a carbonate rock.","Fettes and Desmons, 2007, p195"]
["http://resource.geosciml.org/classifier/cgi/lithology/slate","Slate","Compact, fine grained rock with an average grain size less than 0.032 millimeter and a well developed schistosity (slaty cleavage), and hence can be split into slabs or thin plates.","NADM metamorphic rock vocabulary SLTTm1.0, Neuendorf et al. 2005"]
["http://resource.geosciml.org/classifier/cgi/lithology/spilite","Spilite","Altered basic to intermediate composition fine-grained igneous rock in which the feldspar is partially or completely composed of of albite, typically accompanied by chlorite, calcite, quartz, epidote, prehnite, and low-tempaerature hydrous crystallization products. Preservation of eruptive volcanic features is typical.","Fettes and Desmon, 2007, Best, M.G., 1982, Igneous and metamorphic petrology: New York, W.H. Freeman and Company, p. 398, Neuendorf et al. 2005, p. 619."]
["http://resource.geosciml.org/classifier/cgi/lithology/syenite","Syenite","Syenitic rock that contains between 0 and 5 percent quartz and no feldspathoid mineral in the QAPF fraction. Defined modally in QAPF Field 7.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/syenitic_rock","Syenitic rock","Syenitoid with a plagioclase to total feldspar ratio between 0.1 and 0.35.  Includes rocks in QAPF fields 7, 7*, and 7'.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/syenitoid","Syenitoid","Phaneritic crystalline igneous rock with M less than 90, consisting mainly of alkali feldspar and plagioclase, minor quartz or nepheline may be present, along with pyroxene, amphibole or biotite. Ratio of plagioclase to total feldspar is less than 0.65, quartz forms less than 20 percent of QAPF fraction, and feldspathoid minerals form less than 10 percent of QAPF fraction.  Includes rocks classified in QAPF fields 6, 7 and 8 and their subdivisions.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/syenogranite","Syenogranite","Granite that has a plagiolcase to total feldspar ratio between 0.10 and 0.35. QAPF field 3a.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/tephra","Tephra","Unconsolidated pyroclastic material in which greater than 75 percent of the fragments are deposited as a direct result of volcanic processes and the deposit has not been reworked by epiclastic processes. Includes ash, lapilli tephra, bomb tephra, block tephra and unconsolidated agglomerate.","Hallsworth & Knox 1999, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/tephrite","Tephrite","Tephritoid that has a plagioclase to total feldspar ratio greater than 0.9, and contains less than 10 percent normative (CIPW) olivine.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/tephritic_foidite","Tephritic foidite","Foiditoid that contains less than 90 percent feldspathoid minerals in the QAPF fraction, and has a  plagioclase to total feldspar ratio that is greater than 0.5, with less than 10 percent normative olivine","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/tephritic_phonolite","Tephritic phonolite","Phonolitoid that has a plagioclase to total feldspar ratio between 0.1 and 0.5. Broadly corresponds to TAS tephriphonolite of TAS field U3.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/tephritoid","Tephritoid","Fine grained igneous rock than contains less than 90 percent mafic minerals, between 10 and 60 percent feldspathoid mineral in the QAPF fraction and has a plagioclase to total feldspar ratio greater than 0.5.  Includes rocks classified in QAPF field 13 and 14 or chemically in TAS field U1 as basanite or tephrite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/tholeiitic_basalt","Tholeiitic basalt","Tholeiitic basalt is defined here to contain 2 pyroxene phases and interstitial quartz or tridymite or cristobalite in the groundmass. Pyroxene (augite and orthopyroxene or pigeonite) and calcium-rich plagioclase are common phenocryst minerals. Olivine may also be a phenocryst, and when present, may have rims of pigeonite. Only in tholeiitic basalt is olivine in reaction relationship with melt. Interstitial siliceous residue may be present, and is often glassy. Tholeiitic basalt is relatively poor in sodium.   This category includes most basalts of the ocean floor, most large oceanic islands, and continental flood basalts such as the Columbia River Plateau.","http://en.wikipedia.org/wiki/Basalt, Carmichael, I.S. Turner, F.J., Verhoogen, John, 1974, Igneous petrology: New York, McGraw HIll Book Co., p.42-43."]
["http://resource.geosciml.org/classifier/cgi/lithology/tonalite","Tonalite","Granitoid consisting of quartz and intermediate plagioclase, usually with biotite and amphibole. Includes rocks defined modally in QAPF field 5, ratio of plagioclase to total feldspar is greater than 0.9.^^xsd:string","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/trachyte","Trachyte","Trachytoid that has a plagioclase to total feldspar ratio between 0.1 and 0.35,  between 0 and 5 percent quartz in the QAPF fraction, and no feldspathoid minerals. QAPF field 7.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/trachytic_rock","Trachytic rock","Trachytoid that has a plagioclase to total feldspar ratio between 0.1 and 0.35. QAPF fields 7, 7', and 7*.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/trachytoid","Trachytoid","Fine grained igneous rock than contains less than 90 percent mafic minerals, less than 10 percent feldspathoid mineral and less than 20 percent quartz in the QAPF fraction and has a plagioclase to total feldspar ratio less than 0.65.   Mafic minerals typically include amphibole or mica, typically porphyritic. Includes rocks defined modally in QAPF fields 6, 7 and 8 (with subdivisions) or chemically in TAS Field T as trachyte or latite.","LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/travertine","Travertine","Biotically or abiotically precipitated calcium carbonate, from spring-fedheated, or ambient-temperature water. May be white and spongy, various shades of orange, tan or gray, and ranges to dense, banded or laminated rock. Macrophytes, bryophytes, algae, cyanobacteria and other organisms often colonize the surface of travertine and may be preserved, to produce the porous varieties.","Neuendorf et al. 2005, http://en.wikipedia.org/wiki/Travertine, Chafetzh.S., and Folk, R.L., 1984, Travertine: Depositional morphology an dthe bacterially constructed constituents: J. Sed. Petrology, v. 126, p.57-74."]
["http://resource.geosciml.org/classifier/cgi/lithology/tuff_breccia_agglomerate_or_pyroclastic_breccia","Tuff-breccia, agglomerate, or pyroclastic breccia","Pyroclastic rock in which greater than 25 percent of particles are greater than 64 mm in largest dimension. Includes agglomerate, pyroclastic breccia of Gillespie and Styles (1999)","Schmid 1981, LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/tuffite","Tuffite","Rock consists of more than 50 percent particles of indeterminate pyroclastic or epiclastic origin and less than 75 percent particles of clearly pyroclastic origin. Commonly the rock is laminated or exhibits size grading. (based on LeMaitre et al. 2002, Murawski and Meyer 1998).","LeMaitre et al. 2002, Murawski and Meyer 1998"]
["http://resource.geosciml.org/classifier/cgi/lithology/ultrabasic_igneous_rock","Ultrabasic igneous rock","Igneous rock with less than 45 percent SiO2.","after LeMaitre et al. 2002"]
["http://resource.geosciml.org/classifier/cgi/lithology/ultramafic_igneous_rock","Ultramafic igneous rock","Igneous rock that consists of greater than 90 percent mafic minerals.","LeMaitre et al. 2002, Gillespie and Styles 1999"]
["http://resource.geosciml.org/classifier/cgi/lithology/unconsolidated_material","Unconsolidated material","CompoundMaterial composed of an aggregation of particles that do not adhere to each other strongly enough that the aggregate can be considered a solid in its own right.","This vocabulary"]
["http://resource.geosciml.org/classifier/cgi/lithology/wacke","Wacke","Clastic sandstone with more than 10 percent matrix of indeterminate detrital or diagenetic nature. Matrix is mud size silicate minerals (clay, feldspar, quartz, rock fragments, and alteration products).","Pettijohn, Potter, Siever, 1972, Sand and Sandstone: New York, Springer Verlag, 681 p."]
["http://resource.geosciml.org/classifierscheme/cgi/201202/simplelithology","CGI Simple Lithology Categories","This is the  201202 CGI Simple Lithology vocabulary. Minor comment and bug fixes to definitions and encoding are made in this version. Major change is conversion of URIs to http URI."]