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Seismic activity in the Gulf of Mexico. A preliminary analysis
The southwestern corner of the Gulf of Mexico (around the Isthmus of Tehuantepec) is exposed to intense deep (> 100 km) seismic activity caused by the subduction of the Cocos Plate. Aside from this, the gulf has been considered a zone of low or no-seismicity. However, a sparse shallow seismic act...
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| Publicado no: | Boletín de la Sociedad Geológica Mexicana |
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| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Sociedad Geológica Mexicana, A.C.
2013
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| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=94329954002 |
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