Colorado Potential Geothermal Pathways
Abstract
This layer contains the weakened basement rocks. Isostatic gravity was utilized to identify structural basin areas, characterized by gravity low values reflecting weakened basement rocks. Together interpreted regional fault zones and basin outlines define geothermal "exploration fairways", where the potential exists for deep, superheated fluid flow in the absence of Pliocene or younger volcanic units.
- Authors:
- Publication Date:
- Other Number(s):
- 299
- DOE Contract Number:
- EE0002828
- Research Org.:
- USDOE Geothermal Data Repository (United States); Flint Geothermal, LLC
- Sponsoring Org.:
- USDOE Office of Energy Efficiency and Renewable Energy (EERE), Renewable Power Office. Geothermal Technologies Program (EE-4G)
- Collaborations:
- Flint Geothermal, LLC
- Subject:
- 15 Geothermal Energy
- Keywords:
- geothermal; Colorado; Basement weakness; gravity; faults; fluid flow; Basement weaknesses; ArcGIS; shapefile; shape file; geospatial; geospatial data; data; geophysics; exploration; PFA; play fairway; analysis; superheated fluid flow; volcanic activity; remote sensing; fault detection; anomaly detection
- Geolocation:
- 40.941946633049,-102.0396078125|36.897417334911,-102.0396078125|36.897417334911,-109.19160625|40.941946633049,-109.19160625|40.941946633049,-102.0396078125
- OSTI Identifier:
- 1148766
- DOI:
- https://doi.org/10.15121/1148766
- Project Location:
-
Citation Formats
E., Richard. Colorado Potential Geothermal Pathways. United States: N. p., 2012.
Web. doi:10.15121/1148766.
E., Richard. Colorado Potential Geothermal Pathways. United States. doi:https://doi.org/10.15121/1148766
E., Richard. 2012.
"Colorado Potential Geothermal Pathways". United States. doi:https://doi.org/10.15121/1148766. https://www.osti.gov/servlets/purl/1148766. Pub date:Wed Feb 01 00:00:00 EST 2012
@article{osti_1148766,
title = {Colorado Potential Geothermal Pathways},
author = {E., Richard},
abstractNote = {This layer contains the weakened basement rocks. Isostatic gravity was utilized to identify structural basin areas, characterized by gravity low values reflecting weakened basement rocks. Together interpreted regional fault zones and basin outlines define geothermal "exploration fairways", where the potential exists for deep, superheated fluid flow in the absence of Pliocene or younger volcanic units.},
doi = {10.15121/1148766},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Wed Feb 01 00:00:00 EST 2012},
month = {Wed Feb 01 00:00:00 EST 2012}
}
Save to My Library
You must Sign In or Create an Account in order to save documents to your library.