3D Model of the Neal Hot Springs Geothermal Area

Abstract
The Neal Hot Springs geothermal system lies in a left-step in a north-striking, west-dipping normal fault system, consisting of the Neal Fault to the south and the Sugarloaf Butte Fault to the north (Edwards, 2013). The Neal Hot Springs 3D geologic model consists of 104 faults and 13 stratigraphic units. The stratigraphy is sub-horizontal to dipping <10 degrees and there is no predominant dip-direction. Geothermal production is exclusively from the Neal Fault south of, and within the step-over, while geothermal injection is into both the Neal Fault to the south of the step-over and faults within the step-over.
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Additional Info

DOE 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
DOE Project Number: EE0002748
DOE Project Lead: Mark Ziegenbein
DOI: 10.15121/1136725
Last Updated: over a year ago
Dec
2013
Data from December, 2013
Submitted Mar 21, 2014

University of Nevada

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775.682.8751

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Keywords

geothermal, Neal Hot Springs, 3D Model, Neal Hot Springs Geothermal Area, faulting, stratigraphy, stratigraphic units, cross-section, cross section, faults, geology, geologic units, geologic contact

Status

Publicly accessible License 

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