Paleomagnetic study of Jurassic and Cretaceous rocks north of San Marcos fault, central Coahuila, México
Capas continentales de edad Jurásico Superior y Cretácico Inferior, en el núcleo del anticlinal de la Sierra de La Fragua en el centro de Coahuila, presentan una magnetización característica de polaridad dual, que interpretamos como una magnetización primaria remanente química. Areniscas eólicas y f...
Main Authors: | G. A. González-Naranjo, R. S. Molina Garza, G. Chávez-Cabello |
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Format: | Article |
Language: | English |
Published: |
Universidad Nacional Autónoma de México, Instituto de Geofísica
2008-01-01
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Series: | Geofísica Internacional |
Subjects: | |
Online Access: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/254 |
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