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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Shranjeno v:
Bibliografske podrobnosti
izdano v:Revista Mexicana de Ciencias Geológicas
Main Authors: Lorenzo Meriggi, José Luis Macías, Simone Tommasini, Lucia Capra, Sandro Conticelli
Format: Artigo
Jezik:Inglês
Izdano: Universidad Nacional Autónoma de México 2008
Teme:
Ciencias de la Tierra
high
TiO 2
Trans
Mexico
Volcanic rocks
Online dostop:https://www.redalyc.org/articulo.oa?id=57230346001
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