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Temperature gradient drilling in the Las Cruces East Mesa geothermal field

Journal Article · · Trans. - Geotherm. Resour. Counc.; (United States)
OSTI ID:5097083

Thirty-four shallow temperature gradient holes were drilled on the Las Cruces east mesa adjacent to the Las Alturas geothermal anomaly. Temperature and heat flow data indicate that the anomaly, now named the Las Cruces East Mesa Geothermal Field, is at least 75 km/sup 2/ in size. These data together with geological and geophysical data collected previously suggest that the hydrothermal system is fault controlled and is composed of NW-SE and N-S components, which give the system an apparent NNW-SSE trend.

Research Organization:
New Mexico State University, Energy Institute, Las Cruces, New Mexico
OSTI ID:
5097083
Journal Information:
Trans. - Geotherm. Resour. Counc.; (United States), Journal Name: Trans. - Geotherm. Resour. Counc.; (United States) Vol. 6; ISSN TGRCD
Country of Publication:
United States
Language:
English