Heterogeneous magmas of the Quaternary Sierra Chichinautzin volcanic fi eld (central Mexico): the role of an amphibole-bearing mantle and magmatic evolution processes
The Quaternary Sierra Chichinautzin volcanic fi eld (SCVF) is located at the volcanic front of the Trans-Mexican Volcanic Belt (TMVB), ~350 km from the Middle American trench where the Cocos plate subducts beneath the North American plate. The SCVF is characterized by more than 200 monogenetic cente...
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| Vydáno v: | Revista Mexicana de Ciencias Geológicas |
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| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Nacional Autónoma de México
2008
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=57230346001 |
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