Utah FORGE: Well 16B(78)-32 Drill Core Fracture Analysis Images and Data

Publicly accessible License 

This dataset contains drilling core data from well 16B(78)-32, including PDF documents with flattened core images annotated by feature type and core interval, as well as spreadsheets detailing feature morphologies by depth, planar feature measurements, and planar feature orientations rotated to in situ conditions. Core was recovered from three intervals, one per stimulation stage, in the crystalline rocks affected by the stimulation of well 16A(78)-32. Seven core runs were conducted, yielding 135.8 feet of recovered core.

Features in the core were categorized into planar fractures, semi-planar fractures, unbroken mineralized fractures, rough fractures, curviplanar fractures, concave-convex surfaces, and planar compositional features such as mylonite or dike-like structures. Planar features were measured while the core was positioned horizontally, with the core axis aligned to a downhole azimuth of 42 degrees.

Planar core measurements from stimulations 2 and 3 that could be confidently correlated with FMI data were rotated to in situ orientations. This was done by rotating the planes along vertical and horizontal axes to match the azimuth and inclination data recorded in the directional survey of well 16B(78)-32, as well as applying an axial rotation to resemble the fracture orientations observed in the FMI log at corresponding depths. Coherent sets of planar fracture measurements were made by aligning the core within each 3-foot section of the dissected core barrel, and between adjacent 3-foot sections within a core run by matching rock fabrics, saw cuts and/or tool marks. Where coherent fracture measurements could not be made within a core run, data sets are denoted by a subscript (i.e. 2-Ta and 2-Tb both come from tangent core run number 2).

Citation Formats

Energy and Geoscience Institute at the University of Utah. (2025). Utah FORGE: Well 16B(78)-32 Drill Core Fracture Analysis Images and Data [data set]. Retrieved from https://gdr.openei.org/submissions/1708.
Export Citation to RIS
Jones, Clay. Utah FORGE: Well 16B(78)-32 Drill Core Fracture Analysis Images and Data. United States: N.p., 29 Jan, 2025. Web. https://gdr.openei.org/submissions/1708.
Jones, Clay. Utah FORGE: Well 16B(78)-32 Drill Core Fracture Analysis Images and Data. United States. https://gdr.openei.org/submissions/1708
Jones, Clay. 2025. "Utah FORGE: Well 16B(78)-32 Drill Core Fracture Analysis Images and Data". United States. https://gdr.openei.org/submissions/1708.
@div{oedi_1708, title = {Utah FORGE: Well 16B(78)-32 Drill Core Fracture Analysis Images and Data}, author = {Jones, Clay.}, abstractNote = {This dataset contains drilling core data from well 16B(78)-32, including PDF documents with flattened core images annotated by feature type and core interval, as well as spreadsheets detailing feature morphologies by depth, planar feature measurements, and planar feature orientations rotated to in situ conditions. Core was recovered from three intervals, one per stimulation stage, in the crystalline rocks affected by the stimulation of well 16A(78)-32. Seven core runs were conducted, yielding 135.8 feet of recovered core.

Features in the core were categorized into planar fractures, semi-planar fractures, unbroken mineralized fractures, rough fractures, curviplanar fractures, concave-convex surfaces, and planar compositional features such as mylonite or dike-like structures. Planar features were measured while the core was positioned horizontally, with the core axis aligned to a downhole azimuth of 42 degrees.

Planar core measurements from stimulations 2 and 3 that could be confidently correlated with FMI data were rotated to in situ orientations. This was done by rotating the planes along vertical and horizontal axes to match the azimuth and inclination data recorded in the directional survey of well 16B(78)-32, as well as applying an axial rotation to resemble the fracture orientations observed in the FMI log at corresponding depths. Coherent sets of planar fracture measurements were made by aligning the core within each 3-foot section of the dissected core barrel, and between adjacent 3-foot sections within a core run by matching rock fabrics, saw cuts and/or tool marks. Where coherent fracture measurements could not be made within a core run, data sets are denoted by a subscript (i.e. 2-Ta and 2-Tb both come from tangent core run number 2).
}, doi = {}, url = {https://gdr.openei.org/submissions/1708}, journal = {}, number = , volume = , place = {United States}, year = {2025}, month = {01}}

Details

Data from Jan 29, 2025

Last updated Jan 29, 2025

Submitted Jan 29, 2025

Organization

Energy and Geoscience Institute at the University of Utah

Contact

Clay Jones

801.585.3540

Authors

Clay Jones

Energy and Geoscience Institute at the University of Utah

DOE Project Details

Project Name Utah FORGE

Project Lead Lauren Boyd

Project Number EE0007080

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