Maps, Models and Data from Southeastern Great Basin PFA
Abstract
This submission includes composite risk segment models in raster format for permeability, heat of the earth, and MT, as well as the final PFA model of geothermal exploration risk in Southwestern Utah, USA. Additionally, this submission has data regarding hydrothermally altered areas, and opal sinter deposits in the study area. All of this information lends to the understanding and exploration for hidden geothermal systems in the area.
7 Resources
3 Class Model.zip
This PFA model is probability based and used a heat CRS which included (1) Quaternary basalt flows, (2) Quaternary rhyolite flows and domes, (3) heat flow, (4) Na/K geo... more
This dataset represents the integration of heat data, including heat flow and Na/K geothermometer data, which was used in the Southeastern Great Basin play fairway anal... more
Heat flow data covering part of southwestern utah in the area approximately beteen the Cove Fort geothermal field and the town of Milford. This data was collected by th... more
This dataset represents the probability of rock conductivity being >=0.015, which was used in the Southeastern Great Basin play fairway analysis project, Phase 2, perme... more
The points in this shapefile show locations of silica sinters and hydrothermally altered (opalized/silicified) mio-pliocene fresh water limestone in the Twin Peaks and ... more
This dataset represents the integration of fault density, seismic activity, gravity gradients, and magnetotelluric data that was used in the Southeastern Great Basin pl... more
This excel spreadsheet provides the original x-ray diffraction results from opal samples taken throughout the study area, and given in the accompanying shapefile.
DOE Project Name: Structurally Controlled Geothermal Systems in the Eastern Great Basin Extensional Regime, Utah DOE Project Number: EE0006732 DOE Project Lead: Mike Weathers
DOI: 10.15121/1368062 Last Updated: a year ago
Jun
2017
Data from June, 2017
Submitted Jun 30, 2017
Contact
Energy and Geoscience Institute at the University of Utah
