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 -