Colorado Potential Geothermal Pathways

E., Richard

doi:10.15121/1148766

Title: Colorado Potential Geothermal Pathways

Dataset
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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:

E., Richard

Flint Geothermal, LLC

Publication Date:: Tue Jan 31 23:00:00 EST 2012

Other Number(s):: 299

DOE Contract Number:: EE0002828

Research Org.:: DOE Geothermal Data Repository; 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; ArcGIS; Basement weakness; Basement weaknesses; Colorado; PFA; analysis; anomaly detection; data; exploration; fault detection; faults; fluid flow; geophysics; geospatial; geospatial data; geothermal; gravity; play fairway; remote sensing; shape file; shapefile; superheated fluid flow; volcanic activity

OSTI Identifier:: 1148766

DOI:: https://doi.org/10.15121/1148766

Citation Formats


                    E., Richard. Colorado Potential Geothermal Pathways.  United States: N. p., 2012. 
        Web.  doi:10.15121/1148766.

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                    E., Richard. Colorado Potential Geothermal Pathways.  United States.  doi:https://doi.org/10.15121/1148766

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                    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:Tue Jan 31 23:00:00 EST 2012

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@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         = {Tue Jan 31 23:00:00 EST 2012},

  month        = {Tue Jan 31 23:00:00 EST 2012}

}

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DOI: https://doi.org/10.15121/1148766

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