Colorado Potential Geothermal Pathways

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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.

Citation Formats

Flint Geothermal, LLC. (2012). Colorado Potential Geothermal Pathways [data set]. Retrieved from https://dx.doi.org/10.15121/1148766.
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E., Richard. Colorado Potential Geothermal Pathways. United States: N.p., 01 Feb, 2012. Web. doi: 10.15121/1148766.
E., Richard. Colorado Potential Geothermal Pathways. United States. https://dx.doi.org/10.15121/1148766
E., Richard. 2012. "Colorado Potential Geothermal Pathways". United States. https://dx.doi.org/10.15121/1148766. https://gdr.openei.org/submissions/299.
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https://dx.doi.org/10.15121/1148766

Details

Data from Feb 1, 2012

Last updated Aug 23, 2021

Submitted Feb 26, 2014

Organization

Flint Geothermal, LLC

Contact

Richard E. Zehner

775.737.7806

Authors

Richard E.

Flint Geothermal LLC

DOE Project Details

Project Name Recovery Act: Use Remote Sensing Data (selected visible and infrared spectrums) to locate high temp ground anomalies in Colorado.Confirm heat flow potential w/ on-site temp surveys to drill deep resource wells

Project Lead Mark Ziegenbein

Project Number EE0002828

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