Paleomagnetic study of the Valle de Santiago volcanics, Michoacán-Guanajuato volcanic field, Mexico
The Valle de Santiago area of the Michoacán-Guanajuato volcanic field is characterized by a 7 km by 50 km NNW-SSEtrending cluster of 20 maars, 13 in a smaller sub-area. This volcanic lineament may be associated with a pre-existing fault or zoneof structural weakness, which is approximately normal to...
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| Publicat a: | Geofísica Internacional |
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| Autors principals: | , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Universidad Nacional Autónoma de México
1999
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| Matèries: | |
| Accés en línia: | https://www.redalyc.org/articulo.oa?id=56838402 |
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