Tularosa Basin Play Fairway Analysis: Hydrothermal Alteration Map
Data and Resources
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Hydrothermal Alteration.zipZIP
This is a hydrothermal alteration map of the Tularosa Basin area, New Mexico...
| Field | Value |
|---|---|
| DOI | 10.15121/1261960 |
| accessLevel | public |
| bureauCode | {019:20} |
| catalog_@context | https://openei.org/data.json |
| catalog_@id | https://openei.org/data.json |
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| dataQuality | true |
| identifier | https://data.openei.org/submissions/3402 |
| issued | 2015-11-15T07:00:00Z |
| landingPage | https://gdr.openei.org/submissions/659 |
| license | https://creativecommons.org/licenses/by/4.0/ |
| modified | 2020-01-09T00:10:44Z |
| old-spatial | {"type":"Polygon","coordinates":[[[-106.92227100987,31.434150463543],[-105.30342568908,31.434150463543],[-105.30342568908,34.588590492754],[-106.92227100987,34.588590492754],[-106.92227100987,31.434150463543]]]} |
| programCode | {019:006} |
| projectLead | Mike Weathers |
| projectNumber | EE0006730 |
| projectTitle | Innovative Play Fairway Modelling Applied to the Tularosa Basin |
| publisher | University of Utah |
| resource-type | Dataset |
| source_datajson_identifier | true |
| source_hash | f2c5a5ab1c1b069d2d72dbd5d7753c1f76b97a3f |
| source_schema_version | 1.1 |
| spatial | {"type":"Polygon","coordinates":[[[-106.92227100987,31.434150463543],[-105.30342568908,31.434150463543],[-105.30342568908,34.588590492754],[-106.92227100987,34.588590492754],[-106.92227100987,31.434150463543]]]} |
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| Tags |
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| isopen | True |
| license_id | cc-by |
| license_title | Creative Commons Attribution |
| license_url | http://www.opendefinition.org/licenses/cc-by |
| maintainer | Adam Brandt |
| maintainer_email | u0806276@utah.edu |
| metadata_created | 2025-11-22T04:31:46.995453 |
| metadata_modified | 2025-11-22T04:31:46.995457 |
| notes | This is a hydrothermal alteration map of the Tularosa Basin area, New Mexico and Texas that was created using Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) multispectral data band ratios based upon diagnostic features of clay, calcite, silica, gypsum, ferric iron, and ferrous iron. Mesoproterozoic granite in the San Andreas Range often appeared altered, but this may be from clays produced by weathering or, locally, by hydrothermal alteration. However, no field checking was done. |
| num_resources | 1 |
| num_tags | 23 |
| title | Tularosa Basin Play Fairway Analysis: Hydrothermal Alteration Map |