Newberry Caldera Conceptual Geophysical Model
Conceptual model for the Newberry Caldera geothermal area. Model is centered around caldera and evaluates multiple geophysical datasets to derive a conceptual subsurface model.
Includes:
Conductor layer based on transient electromagnetic data from Fitterman et al., 1988 (figure 10)
Base of conductor layer based on MT conductor values found in Waibel et al., 2014 (DOE document, figure 38)
Resistor layer based on magnetotellurics from Fitterman et al., 1988 (figure 13).
Seismic intrusives layer representing a smoothed version of 5.5 km/s seismic velocity layer defined in Beachly et al., 2012
West flank seismic body representing a fractional change in seismic velocity of 0.1, defined in Beachly et al., 2012 and Heath et al., 2015
West flank gravity body "granite" that represents a gravity anomaly identified in Waibel et al., 2014 (DOE document, figure 35)
Magma chamber defined seismically, found in Heath et al., 2015
Ring fracture fault intrusions
Various faults and geologic layers
Citation Formats
National Energy Technology Laboratory. (2016). Newberry Caldera Conceptual Geophysical Model [data set]. Retrieved from https://gdr.openei.org/submissions/752.
Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., and Vincent, P. Newberry Caldera Conceptual Geophysical Model. United States: N.p., 04 Mar, 2016. Web. https://gdr.openei.org/submissions/752.
Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., & Vincent, P. Newberry Caldera Conceptual Geophysical Model. United States. https://gdr.openei.org/submissions/752
Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., and Vincent, P. 2016. "Newberry Caldera Conceptual Geophysical Model". United States. https://gdr.openei.org/submissions/752.
@div{oedi_752, title = {Newberry Caldera Conceptual Geophysical Model}, author = {Moser, Mark M., Schultz, J., Schultz, A., Heath, B., Rose, Kelly, Urquhart, S., Bowles-Martinez, E., and Vincent, P.}, abstractNote = {Conceptual model for the Newberry Caldera geothermal area. Model is centered around caldera and evaluates multiple geophysical datasets to derive a conceptual subsurface model.
Includes:
Conductor layer based on transient electromagnetic data from Fitterman et al., 1988 (figure 10)
Base of conductor layer based on MT conductor values found in Waibel et al., 2014 (DOE document, figure 38)
Resistor layer based on magnetotellurics from Fitterman et al., 1988 (figure 13).
Seismic intrusives layer representing a smoothed version of 5.5 km/s seismic velocity layer defined in Beachly et al., 2012
West flank seismic body representing a fractional change in seismic velocity of 0.1, defined in Beachly et al., 2012 and Heath et al., 2015
West flank gravity body "granite" that represents a gravity anomaly identified in Waibel et al., 2014 (DOE document, figure 35)
Magma chamber defined seismically, found in Heath et al., 2015
Ring fracture fault intrusions
Various faults and geologic layers }, doi = {}, url = {https://gdr.openei.org/submissions/752}, journal = {}, number = , volume = , place = {United States}, year = {2016}, month = {03}}
Details
Data from Mar 4, 2016
Last updated Nov 14, 2019
Submitted Apr 1, 2016
Organization
National Energy Technology Laboratory
Contact
Kelly Rose
Authors
Keywords
geothermal, enhanced geothermal system, EGS, NEWGEN, Newberry, Oregon, gravity, seismic, conceptual model, subsurface model, geologic model, structure, geophysics, faults, MT, magnetotelluric, model, conceptual, geophysical, calderaDOE Project Details
Project Name Novel use of 4D Monitoring Techniques to Improve Reservoir Longevity and Productivity in Enhanced Geothermal Systems
Project Lead Lauren Boyd
Project Number FY11 AOP 11113