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Evolution of the geometry of normal faults in the Oligocene volcanic field of the Mesa Central, Mexico
We document that the direction of fault traces and the long axis of volcanic domes show a similar distribution, which indicates that the normal faults controlled in some way the location of volcanic rocks. In this study we analyze the evolution of the faults from a geometric point of view, without c...
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| Publicado no: | Boletín de la Sociedad Geológica Mexicana |
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| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Espanhol |
| Publicado em: |
Sociedad Geológica Mexicana, A.C.
2008
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| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=94316033005 |
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