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    Data from: Structural Data for the Columbus Salt Marsh Geothermal Area - GIS...

    • catalog.data.gov
    • gdr.openei.org
    • +1more
    Updated Jan 20, 2025
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    University of Nevada (2025). Structural Data for the Columbus Salt Marsh Geothermal Area - GIS Data [Dataset]. https://catalog.data.gov/dataset/structural-data-for-the-columbus-salt-marsh-geothermal-area-gis-data-01ea7
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    Dataset updated
    Jan 20, 2025
    Dataset provided by
    University of Nevada
    Area covered
    Columbus Marsh
    Description

    Shapefiles and spreadsheets of structural data, including attitudes of faults and strata and slip orientations of faults. - Detailed geologic mapping of ~30 km2 was completed in the vicinity of the Columbus Marsh geothermal field to obtain critical structural data that would elucidate the structural controls of this field. - Documenting E- to ENE-striking left lateral faults and N- to NNE-striking normal faults. - Some faults cut Quaternary basalts. - This field appears to occupy a displacement transfer zone near the eastern end of a system of left-lateral faults. ENE-striking sinistral faults diffuse into a system of N- to NNE-striking normal faults within the displacement transfer zone. - Columbus Marsh therefore corresponds to an area of enhanced extension and contains a nexus of fault intersections, both conducive for geothermal activity.

  2. Data from: Structural Data for the Columbus Salt Marsh Geothermal Area - GIS...

    • osti.gov
    Updated Dec 31, 2011
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    Faulds, James E. (2011). Structural Data for the Columbus Salt Marsh Geothermal Area - GIS Data [Dataset]. https://www.osti.gov/dataexplorer/biblio/dataset/1136716
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    Dataset updated
    Dec 31, 2011
    Dataset provided by
    United States Department of Energyhttp://energy.gov/
    Office of Energy Efficiency and Renewable Energyhttp://energy.gov/eere
    USDOE Geothermal Data Repository (United States); University of Nevada Reno
    Authors
    Faulds, James E.
    Area covered
    Columbus Marsh
    Description

    Shapefiles and spreadsheets of structural data, including attitudes of faults and strata and slip orientations of faults. - Detailed geologic mapping of ~30 km2 was completed in the vicinity of the Columbus Marsh geothermal field to obtain critical structural data that would elucidate the structural controls of this field. - Documenting E‐ to ENE‐striking left lateral faults and N‐ to NNE‐striking normal faults. - Some faults cut Quaternary basalts. - This field appears to occupy a displacement transfer zone near the eastern end of a system of left‐lateral faults. ENE‐striking sinistral faults diffuse into a system of N‐ to NNE‐striking normal faults within the displacement transfer zone. - Columbus Marsh therefore corresponds to an area of enhanced extension and contains a nexus of fault intersections, both conducive for geothermal activity.

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Click to copy link
Link copied
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University of Nevada (2025). Structural Data for the Columbus Salt Marsh Geothermal Area - GIS Data [Dataset]. https://catalog.data.gov/dataset/structural-data-for-the-columbus-salt-marsh-geothermal-area-gis-data-01ea7

Data from: Structural Data for the Columbus Salt Marsh Geothermal Area - GIS Data

Related Article
Explore at:
Dataset updated
Jan 20, 2025
Dataset provided by
University of Nevada
Area covered
Columbus Marsh
Description

Shapefiles and spreadsheets of structural data, including attitudes of faults and strata and slip orientations of faults. - Detailed geologic mapping of ~30 km2 was completed in the vicinity of the Columbus Marsh geothermal field to obtain critical structural data that would elucidate the structural controls of this field. - Documenting E- to ENE-striking left lateral faults and N- to NNE-striking normal faults. - Some faults cut Quaternary basalts. - This field appears to occupy a displacement transfer zone near the eastern end of a system of left-lateral faults. ENE-striking sinistral faults diffuse into a system of N- to NNE-striking normal faults within the displacement transfer zone. - Columbus Marsh therefore corresponds to an area of enhanced extension and contains a nexus of fault intersections, both conducive for geothermal activity.

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