Origin of bimodal rear‐arc volcanism, <scp>Trans‐Mexican</scp> Volcanic Belt eastern sector: Geochemical and isotopic evidence from the Quaternary <scp>Xihuingo‐La</scp> Paila Volcanic Field-Reference-Cited by-同舟云学术

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Origin of bimodal rear‐arc volcanism, Trans‐Mexican Volcanic Belt eastern sector: Geochemical and isotopic evidence from the Quaternary Xihuingo‐La Paila Volcanic Field

Published:2022-01-10 Issue:5 Volume:57 Page:1957-1977
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Martínez‐Serrano Raymundo G.¹^ORCID,Valadez‐Cabrera Sac‐Nicté²,Roberge Julie³^ORCID,Cristiani‐Solís Carlos G.²

Affiliation:

1. Instituto de Geofísica, Laboratorio Universitario de Geoquímica Isotópica (LUGIS‐LANGEM), Universidad Nacional Autónoma de México Ciudad de México Mexico

2. Posgrado en Ciencias de la Tierra, Universidad Nacional Autónoma de México Ciudad de México Mexico

3. Escuela Superior de Ingeniería, Instituto Politécnico Nacional Ciudad de México Mexico

Funder

Dirección General de Asuntos del Personal Académico, Universidad Nacional Autónoma de México

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4390

Reference92 articles.

1. Geology and geochemistry of Pelagatos, Cerro del Agua, and Dos Cerros monogenetic volcanoes in the Sierra Chichinautzin Volcanic Field, south of México City

2. The Genesis of Intermediate and Silicic Magmas in Deep Crustal Hot Zones

3. Generation of sodium-rich magmas from newly underplated basaltic crust

4. Distinct site preferences for heavy and light REE in amphibole and the prediction of Amph/L D REE

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