Shallow crustal structure of the junction of the grabens of Chapala, Tepic-Zacoalco and Colima, Mexico

Gravity data is used to infer the shallow crustal structure of the Tepic graben adjacent to the City of Guadalajara. This depression does not constitute a symmetric graben with steep master faults but rather a complex transition zone. Blocks detached from the granitic sierras are downfaulted and til...

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Bibliographic Details
Main Authors: J. O. Campos-Enríquez, M.A. Alatorre-Zamora
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México, Instituto de Geofísica 1998-06-01
Series:Geofísica Internacional
Subjects:
Online Access:http://www.geofisica.unam.mx/unid_apoyo/editorial/publicaciones/investigacion/geofisica_internacional/anteriores/1998/04/campos.pdf