3D Model of the San Emidio Geothermal Area

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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Additional Info

Field Value
Source https://gdr.openei.org/submissions/365
Author University of Nevada
Maintainer James E. Faulds
bureau_code 019:20
Catalog GDR
Contact Phone 775.682.8751
harvest_object_id 560c86e3-3eb2-49d9-b966-50bb713c30cb
harvest_source_id 154c8289-1404-4e71-a217-a08000129ad0
harvest_source_title Geothermal Data Repository (GDR)
Origination Date 2013-12-31
program_code 019:006
Sectors Geothermal
was_harvested true

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