Heterogeneous magmas of the Quaternary Sierra Chichinautzin volcanic field (central Mexico): the role of an amphibole-bearing mantle and magmatic evolution processes

Heterogeneous magmas of the Quaternary Sierra Chichinautzin volcanic field (central Mexico): the role of an amphibole-bearing mantle and magmatic evolution processes

The Quaternary Sierra Chichinautzin volcanic field (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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Bibliographic Details
Main Authors: Lorenzo Meriggi, José Luis Luis Macías, Simone Tommasini, Lucia Capra, Sandro Conticelli
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México 2018-01-01
Series:Revista Mexicana de Ciencias Geológicas
Subjects:
volcanic rocks
high-TiO2
Sr and Nd isotopes
magmatic evolution
Sierra Chichinautzin
Trans-Mexican Volcanic Belt
Online Access:https://rmcg.unam.mx/index.php/rmcg/article/view/652
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