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Curie point depth from spectral analysis of aeromagnetic data from Cerro Prieto geothermal area,Baja California,México
Authors:JM Espinosa-Cardeña  JO Campos-Enriquez
Institution:1. Departamente de Geofísica Aplicada, Centro de Investigación y Estudios Superiores de Ensenada, B.C., Km 107 carretera Tijuana-Ensenada, Mexico;2. Instituto de Geofisica, UNAM, Deleg. Coyoacan, 04510 México, D.F., Mexico
Abstract:Using aeromagnetic data acquired in the area from the Cerro Prieto geothermal field, we estimated the depth to the Curie point isotherm, interpreted as the base of the magnetic sources, following statistical spectral-based techniques. According to our results the Curie point isotherm is located at a depths ranging from 14 to 17 km. Our result is somewhat deeper than that obtained previously based only in 2-D and 3-D forward modeling of previous low-quality data. However, our results are supported by independent information comprising geothermal gradients, seismicity distribution in the crust, and gravity determined crustal thickness. Our results imply a high thermal gradient (ranging between 33 and 38 °C/km) and high heat flow (of about 100 mW/m2) for the study area. The thermal regime for the area is inferred to be similar to that from the Salton trough.
Keywords:Curie point temperature  depth to base of magnetic sources  aeromagnetic data  spectral&ndash  statistical techniques  Cerro Prieto geothermal field (Mexico)
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