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3D Model of the San Emidio Geothermal Area

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The San Emidio geothermal system is characterized by a left-step in a west-dipping normal fault system that bounds the western side of the Lake Range. The 3D geologic model consists of 5 geologic units and 55 faults. Overlying Jurrassic-Triassic metasedimentary basement is a ~500 m-1000 m thick section of the Miocene lower Pyramid sequence, pre- syn-extensional Quaternary sedimentary rocks and post-extensional Quaternary rocks. 15-30 degrees eastward dip of the stratigraphy is controlled by the predominant west-dipping fault set. Both geothermal production and injection are concentrated north of the step over in an area of closely spaced west dipping normal faults.

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TY - DATA AB - The San Emidio geothermal system is characterized by a left-step in a west-dipping normal fault system that bounds the western side of the Lake Range. The 3D geologic model consists of 5 geologic units and 55 faults. Overlying Jurrassic-Triassic metasedimentary basement is a ~500 m-1000 m thick section of the Miocene lower Pyramid sequence, pre- syn-extensional Quaternary sedimentary rocks and post-extensional Quaternary rocks. 15-30 degrees eastward dip of the stratigraphy is controlled by the predominant west-dipping fault set. Both geothermal production and injection are concentrated north of the step over in an area of closely spaced west dipping normal faults. AU - E., James DB - Open Energy Data Initiative (OEDI) DP - Open EI | National Renewable Energy Laboratory DO - 10.15121/1136724 KW - geothermal KW - San Emidio Geothermal Area KW - 3D Model KW - San Emidio KW - faulting KW - stratigraphy KW - stratigraphic units KW - faults KW - cross-section KW - cross section KW - geology KW - geologic units KW - geologic contact KW - data KW - geospatial data LA - English DA - 2013/12/31 PY - 2013 PB - University of Nevada T1 - 3D Model of the San Emidio Geothermal Area UR - https://doi.org/10.15121/1136724 ER -
Export Citation to RIS
E., James. 3D Model of the San Emidio Geothermal Area. University of Nevada, 31 December, 2013, GDR. https://doi.org/10.15121/1136724.
E., J. (2013). 3D Model of the San Emidio Geothermal Area. [Data set]. GDR. University of Nevada. https://doi.org/10.15121/1136724
E., James. 3D Model of the San Emidio Geothermal Area. University of Nevada, December, 31, 2013. Distributed by GDR. https://doi.org/10.15121/1136724
@misc{OEDI_Dataset_6702, title = {3D Model of the San Emidio Geothermal Area}, author = {E., James}, abstractNote = {The San Emidio geothermal system is characterized by a left-step in a west-dipping normal fault system that bounds the western side of the Lake Range. The 3D geologic model consists of 5 geologic units and 55 faults. Overlying Jurrassic-Triassic metasedimentary basement is a ~500 m-1000 m thick section of the Miocene lower Pyramid sequence, pre- syn-extensional Quaternary sedimentary rocks and post-extensional Quaternary rocks. 15-30 degrees eastward dip of the stratigraphy is controlled by the predominant west-dipping fault set. Both geothermal production and injection are concentrated north of the step over in an area of closely spaced west dipping normal faults.}, url = {https://gdr.openei.org/submissions/365}, year = {2013}, howpublished = {GDR, University of Nevada, https://doi.org/10.15121/1136724}, note = {Accessed: 2025-05-04}, doi = {10.15121/1136724} }
https://dx.doi.org/10.15121/1136724

Details

Data from Dec 31, 2013

Last updated Aug 27, 2021

Submitted Mar 21, 2014

Organization

University of Nevada

Contact

James E. Faulds

775.682.8751

Authors

James E.

University of Nevada

Research Areas

DOE Project Details

Project Name Recovery Act: Characterizing Structural Controls of EGS-Candidate and Conventional Geothermal Reservoirs in the Great Basin: Developing Successful Exploration Strategies in Extended Terranes

Project Lead Mark Ziegenbein

Project Number EE0002748

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