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General Overview of Geophysical Studies at Cerro Prieto

Goldstein, N. E.

Location
Cerro Prieto, Mexico
Conference
DOE-CFE Symposium on Cerro Prieto
Year
1978
Session
Geophysics/Geofisica
Language
English, Spanish

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Abstract

A tectonically active region of the earth's crust having scientific bearing on plate tectonic theory, the Salton Trough has been under study by geophysicists for many years (Kovach et al., 1962; Biehler, et al., 1964). Interest in the Mexicali Valley portion of the trough and in Cerro Prieto for geothermal energy development, began about 20 years ago (Reed, 1976).

La Depresion de Salton, como region tectonicamente activa de la corteza terrestre relacionada cientfficamente con la teoria de tectonica de placas, ha side estudiada por geofisicos durante muchos anos (Kovach y otros, 1962; Biehler y otros, 1964). Hace aproximadamente veinte anos surgio el interes en la parte de la depresion correspondiente al Valle de Mexicali y a Cerro Prieto, para el desarrollo de energia geotermica (Reed, 1976).

Copyright 1978, DOE-CFE Symposium on Cerro Prieto. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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