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Title: 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.

Authors:
Publication Date:
Other Number(s):
364
DOE Contract Number:  
EE0002748
Product Type:
Dataset
Research Org.:
DOE Geothermal Data Repository; University of Nevada Reno
Sponsoring Org.:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Office
Subject:
15 Geothermal Energy
Keywords:
geothermal; Neal Hot Springs; 3D Model; Neal Hot Springs Geothermal Area
OSTI Identifier:
1136725
DOI:
10.15121/1136725

Citation Formats

Faulds, James E. 3D Model of the Neal Hot Springs Geothermal Area. United States: N. p., 2013. Web. doi:10.15121/1136725.
Faulds, James E. 3D Model of the Neal Hot Springs Geothermal Area. United States. doi:10.15121/1136725.
Faulds, James E. 2013. "3D Model of the Neal Hot Springs Geothermal Area". United States. doi:10.15121/1136725. https://www.osti.gov/servlets/purl/1136725. Pub date:Tue Dec 31 00:00:00 EST 2013
@article{osti_1136725,
title = {3D Model of the Neal Hot Springs Geothermal Area},
author = {Faulds, James E.},
abstractNote = {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.},
doi = {10.15121/1136725},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2013},
month = {12}
}

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