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Structural Inventory of Great Basin Geothermal Systems and Definition of Favorable Structural Settings
Structural controls of 426 geothermal systems in the Great Basin region including western Nevada, central Nevada, northwestern Nevada, northeastern Nevada, east-central Nevada, eastern California, southern Oregon, and western Utah were analyzed with literature research, air photos...
Faulds, J. University of Nevada
Dec 31, 2013
1 Resources
0 Stars
Publicly accessible
1 Resources
0 Stars
Publicly accessible
Geologic Map of the Neal Hot Springs Geothermal Area GIS Data
Neal Hot Springs-ESRI Geodatabase (ArcGeology v1.3):
Contains all the geologic map data, including faults, contacts, folds, unit polygons,
and attitudes of strata and faults.
List of stratigraphic units and stratigraphic correlation diagram.
Three cross-sections.
Locations of ...
E., J. University of Nevada
Mar 31, 2013
1 Resources
0 Stars
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1 Resources
0 Stars
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Geologic Map and GIS Data for the Patua Geothermal Area
Patua-ESRI Geodatabase (ArcGeology v1.3):
Contains all the geologic map data, including faults, contacts, folds, veins, dikes, unit polygons, and attitudes of strata and faults.
List of stratigraphic units.
Locations of geothermal wells.
Locations of 40Ar/39Ar and tephra samples.
E., J. University of Nevada
Oct 31, 2011
1 Resources
0 Stars
Publicly accessible
1 Resources
0 Stars
Publicly accessible
Geologic Map and GIS Data for the Salt Wells Geothermal Area
Salt Wells-ESRI Geodatabase (ArcGeology v1.3):
Contains all the geologic map data, including faults, contacts, folds, dikes, unit polygons, and attitudes of strata and faults.
List of stratigraphic units and stratigraphic correlation diagram.
Locations of 40Ar/39Ar samples.
Hinz, N. University of Nevada
Oct 31, 2011
1 Resources
0 Stars
Publicly accessible
1 Resources
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3D Model of the Neal Hot Springs Geothermal Area
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...
E., J. University of Nevada
Dec 31, 2013
1 Resources
0 Stars
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1 Resources
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Structural Controls of the Neal Hot Springs Geothermal System, Eastern Oregon
Detailed geologic mapping (1:24,000 scale), structural and geochemical analyses, and integration of available geophysical and well-field data were utilized to assess the structural controls of the Neal Hot Springs geothermal field in eastern Oregon. The geothermal field lies withi...
Edwards, J. and Faulds, J. University of Nevada
May 31, 2013
1 Resources
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1 Resources
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Slip and Dilation Tendency Analysis of Neal Hot Springs Geothermal Area
Slip and Dilation Tendency in focus areas
Critically stressed fault segments have a relatively high likelihood of acting as fluid flow conduits (Sibson, 1994). As such, the tendency of a fault segment to slip (slip tendency; Ts; Morris et al., 1996) or to dilate (dilation tendency...
E., J. University of Nevada
Dec 31, 2013
1 Resources
0 Stars
Publicly accessible
1 Resources
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Geologic Map and GIS Data for the Wabuska Geothermal Area
Wabuska-ESRI geodatabase (ArcGeology v1.3):
Contains all the geologic map data, including faults, contacts, folds, veins, dikes, unit polygons, and attitudes of strata.
List of stratigraphic units and stratigraphic correlation diagram.
One cross-section.
Hinz, N. University of Nevada
Sep 30, 2013
1 Resources
0 Stars
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1 Resources
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Brady's Field GPS RINEX Files 12-20-2014
CSV files with links to individual GPS RINEX files.
Kreemer, C. University of Nevada
Dec 20, 2014
4 Resources
0 Stars
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4 Resources
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Brady's Field GPS Time-Series Data
Daily position time-series for GPS station BRAD and BRDY in the NA12 reference frame.
Kreemer, C. University of Nevada
Dec 20, 2014
1 Resources
0 Stars
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1 Resources
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PoroTomo Project: Brady's Geothermal Field: GPS station deployment and data analysis
Brady's Field PoroTomo project. GPS station deployment and data analysis. Links to data files and website with station and time-series information
Kreemer, C. University of Nevada
Apr 26, 2016
8 Resources
0 Stars
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8 Resources
0 Stars
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Slip and Dilation Tendency Analysis of the Patua Geothermal Area
Critically stressed fault segments have a relatively high likelihood of acting as fluid flow conduits (Sibson, 1994). As such, the tendency of a fault segment to slip or to dilate provides an indication of which faults or fault segments within a geothermal system are critically st...
E., J. University of Nevada
Dec 31, 2013
1 Resources
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1 Resources
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Structural Controls of the Tuscarora Geothermal Field, Elko County, Nevada MS Thesis
Detailed geologic mapping, structural analysis, and well data have been integrated to elucidate the stratigraphic framework and structural setting of the Tuscarora geothermal area. Tuscarora is an amagmatic geothermal system that lies in the northern part of the Basin and Range pr...
Dering, G. and Faulds, J. University of Nevada
May 31, 2013
1 Resources
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1 Resources
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Slip and Dilation Tendency Analysis of the Salt Wells Geothermal Area
Critically stressed fault segments have a relatively high likelihood of acting as fluid flow conduits (Sibson, 1994). As such, the tendency of a fault segment to slip (slip tendency; Ts; Morris et al., 1996) or to dilate (dilation tendency; Td; Ferrill et al., 1999) provides an in...
E., J. University of Nevada
Dec 31, 2013
1 Resources
0 Stars
Publicly accessible
1 Resources
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Publicly accessible
Slip and Dilation Tendency Analysis of the San Emidio Geothermal Area
Critically stressed fault segments have a relatively high likelihood of acting as fluid flow conduits (Sibson, 1994). As such, the tendency of a fault segment to slip (slip tendency; Ts; Morris et al., 1996) or to dilate (dilation tendency; Td; Ferrill et al., 1999) provides an in...
E., J. University of Nevada
Dec 31, 2013
1 Resources
0 Stars
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1 Resources
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Slip and Dilation Tendency Analysis of McGinness Hills Geothermal Area
Slip and Dilation Tendency in focus areas
Critically stressed fault segments have a relatively high likelihood of acting as fluid flow conduits (Sibson, 1994). As such, the tendency of a fault segment to slip (slip tendency; Ts; Morris et al., 1996) or to dilate (dilation tendency...
E., J. University of Nevada
Dec 31, 2013
1 Resources
0 Stars
Publicly accessible
1 Resources
0 Stars
Publicly accessible
Slip and Dilation Tendency Analysis of the Tuscarora Geothermal Area
Critically stressed fault segments have a relatively high likelihood of acting as fluid flow conduits (Sibson, 1994). As such, the tendency of a fault segment to slip (slip tendency; Ts; Morris et al., 1996) or to dilate (dilation tendency; Td; Ferrill et al., 1999) provides an in...
E., J. University of Nevada
Dec 31, 2013
1 Resources
0 Stars
Publicly accessible
1 Resources
0 Stars
Publicly accessible