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Colorado Potential Geothermal Pathways
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.
Complete Metadata
| bureauCode |
[ "019:20" ] |
|---|---|
| dataQuality | true |
| DOI | 10.15121/1148766 |
| identifier | https://data.openei.org/submissions/6637 |
| issued | 2012-02-01T07:00:00Z |
| landingPage | https://gdr.openei.org/submissions/299 |
| programCode |
[ "019:006" ] |
| projectLead | Mark Ziegenbein |
| projectNumber | EE0002828 |
| projectTitle | 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 |
| spatial | {"type":"Polygon","coordinates":[[[-109.19160625,36.897417334911],[-102.0396078125,36.897417334911],[-102.0396078125,40.941946633049],[-109.19160625,40.941946633049],[-109.19160625,36.897417334911]]]} |
