Modeling the marine magnetic field of Bahía de Banderas, Mexico, confirms the half-graben structure of the bay

Author:

Alvarez Román,López-Loera Héctor,Arzate Jorge

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference37 articles.

1. Geology of the northern Colima and Zacoalco grabens, southwest Mexico: late Cenozoic rifting in the Mexican Volcanic Belt;Allan;GSA Bull.,1986

2. Pliocene–Holocene rifting and associated volcanism in southwest Mexico: an exotic terrane in the making;Allan,1991

3. Banderas rift zone: a plausible NW limit of the Jalisco block;Alvarez;Geophys. Res. Lett.,2002

4. Submarine topography and faulting in Bahía de Banderas, Mexico;Alvarez;Geofísica Int.,2007

5. Geophysical modeling of Valle de Banderas graben and its structural relation to Bahía de Banderas, Mexico;Arzate;Rev. Mex. C. Geológicas,2006

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