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Title: Tularosa Basin Play Fairway Analysis: Hydrothermal Alteration Map

Abstract

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. This work was done under U.S. D.O.E. Contract #DE-EE0006730

Creator(s)/Author(s):
Publication Date:
Other Number(s):
659
DOE Contract Number:  
EE0006730
Product Type:
Dataset
Research Org.:
DOE Geothermal Data Repository; University of Utah
Sponsoring Org.:
USDOE Office of Energy Efficiency and Renewable Energy (EERE), Geothermal Technologies Program (EE-2C)
Subject:
15 Geothermal Energy
Keywords:
geothermal; Tularosa; Basin; Hydrothermal; alteration; map; texas; new mexico; play fairway analysis; tularosa; hydrothermal; basin; pfa
OSTI Identifier:
1261960
DOI:
10.15121/1261960

Citation Formats

Brandt, Adam. Tularosa Basin Play Fairway Analysis: Hydrothermal Alteration Map. United States: N. p., 2015. Web. doi:10.15121/1261960.
Brandt, Adam. Tularosa Basin Play Fairway Analysis: Hydrothermal Alteration Map. United States. doi:10.15121/1261960.
Brandt, Adam. 2015. "Tularosa Basin Play Fairway Analysis: Hydrothermal Alteration Map". United States. doi:10.15121/1261960. https://www.osti.gov/servlets/purl/1261960. Pub date:Sun Nov 15 00:00:00 EST 2015
@article{osti_1261960,
title = {Tularosa Basin Play Fairway Analysis: Hydrothermal Alteration Map},
author = {Brandt, Adam},
abstractNote = {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. This work was done under U.S. D.O.E. Contract #DE-EE0006730},
doi = {10.15121/1261960},
journal = {},
number = ,
volume = ,
place = {United States},
year = {2015},
month = {11}
}

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