Geometry and state of stress of the Wadati-Benioff zone in the Gulf of Tehuantepec, Mexico

Author:

Bravo Hugo1,Rebollar Cecilio J.2,Uribe Antonio1,Jimenez Oscar1

Affiliation:

1. Gerencia de Estudios de Ingenieria Civil, Departamento de Sismotectonica; Mexico D. F. Mexico

2. Centro de Investigacion Cientifica y Educacion Superior de Ensenada (CICESE), Ensenada; Baja California Mexico

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference40 articles.

1. A preliminary crustal model of the Oaxaca continental margin and subduction zone from magnetotelluric and gravity measurements;Arzate;Geofis. Int.,1993

2. Large intermediate-depth earthquakes and the subduction process;Astiz;Phys. Earth Planet. Inter.,1988

3. Neotectonic evolution of the Isthmus of Tehuantepec (southern Mexico);Barrier;Tectonophysics,1998

4. Tectonostratigraphic terranes and mineral resources distribution in Mexico;Campa;Can. J. Earth Sci.,1983

5. Gravity and structure of the continental margins of southwestern Mexico and northwestern Guatemala;Couch;J. Geophys. Res.,1981

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