A seismic and gravity study of the McGregor geothermal system, southern New Mexico

摘要

Seismic and gravity studies have proven to be valu- able tools in evaluating the geologic setting and eco- nomic potential of the McGregor geothermal system of southern New Mexico. An initial gravity study of tem demonstrated that a gravity high coincides with the heat-flow high. A subsequent seismic reflection survey images a strong reflector, interpreted to be associated with a bedrock high that underlies the gravity and heat- flow highs.