Hydrothermal mineral alterations in the Brady and Desert Peak geothermal fields

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Results of the analysis of HyMap's spectra against know hydrothermally altered minerals in the Brady-Desert Peak Geothermal Areas. The analysis was performed using ENVI's Target Detection process against USGS library spectra for Chalcedony, Kaolinite, Gypsum, Hematite and Epsomite.
Each compressed file includes three raster images created after fusing the target detection results for all minerals:
_fusion_all - Contains the 8 layers resulting from target detection and fusion of the 5 minerals
_fusion_all_normal - Contains each layer as above, after Winsorization (99% percentile on the positive side only due to skewness of results), and normalization of each layer to achieve a range between [0-1]
_fusion_final - Contains a fused raster by sub-setting the normalized layers, with the results of MTMF, MTTCIMF, OSP and SAM. Both CEM and MF were discarded as being less accurate than MTMF, and TCIMF is less accurate than MTTCIMF, ACE results were discarded because they were notably different from the rest of the analyses.

The base_names are:
brady - Brady geothermal area only
desert - Desert Peak geothermal area only
hymap - Full image analysis comprising both the Brady and Desert Peak geothermal areas

Citation Formats

Colorado School of Mines. (2021). Hydrothermal mineral alterations in the Brady and Desert Peak geothermal fields [data set]. Retrieved from https://dx.doi.org/10.15121/1824162.
Export Citation to RIS
Moraga, Jim. Hydrothermal mineral alterations in the Brady and Desert Peak geothermal fields. United States: N.p., 01 Oct, 2021. Web. doi: 10.15121/1824162.
Moraga, Jim. Hydrothermal mineral alterations in the Brady and Desert Peak geothermal fields. United States. https://dx.doi.org/10.15121/1824162
Moraga, Jim. 2021. "Hydrothermal mineral alterations in the Brady and Desert Peak geothermal fields". United States. https://dx.doi.org/10.15121/1824162. https://gdr.openei.org/submissions/1334.
@div{oedi_1334, title = {Hydrothermal mineral alterations in the Brady and Desert Peak geothermal fields}, author = {Moraga, Jim.}, abstractNote = {Results of the analysis of HyMap's spectra against know hydrothermally altered minerals in the Brady-Desert Peak Geothermal Areas. The analysis was performed using ENVI's Target Detection process against USGS library spectra for Chalcedony, Kaolinite, Gypsum, Hematite and Epsomite.
Each compressed file includes three raster images created after fusing the target detection results for all minerals:
_fusion_all - Contains the 8 layers resulting from target detection and fusion of the 5 minerals
_fusion_all_normal - Contains each layer as above, after Winsorization (99% percentile on the positive side only due to skewness of results), and normalization of each layer to achieve a range between [0-1]
_fusion_final - Contains a fused raster by sub-setting the normalized layers, with the results of MTMF, MTTCIMF, OSP and SAM. Both CEM and MF were discarded as being less accurate than MTMF, and TCIMF is less accurate than MTTCIMF, ACE results were discarded because they were notably different from the rest of the analyses.

The base_names are:
brady - Brady geothermal area only
desert - Desert Peak geothermal area only
hymap - Full image analysis comprising both the Brady and Desert Peak geothermal areas
}, doi = {10.15121/1824162}, url = {https://gdr.openei.org/submissions/1334}, journal = {}, number = , volume = , place = {United States}, year = {2021}, month = {10}}
https://dx.doi.org/10.15121/1824162

Details

Data from Oct 1, 2021

Last updated Oct 6, 2021

Submitted Oct 2, 2021

Organization

Colorado School of Mines

Contact

Jim Moraga

303.273.3768

Authors

Jim Moraga

Colorado School of Mines

DOE Project Details

Project Name Detection of Potential Geothermal Exploration Sites from Hyperspectral Images via Deep Learning

Project Lead Mike Weathers

Project Number EE0008760

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