Heterogeneous dacitic magmas and the role of crustal assimilation in the Sierra Chichinautzin Volcanic Field, central Mexico: a perspective from crustal xenoliths-Reference-Cited by-同舟云学术

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Heterogeneous dacitic magmas and the role of crustal assimilation in the Sierra Chichinautzin Volcanic Field, central Mexico: a perspective from crustal xenoliths

Published:2024-03-04 Issue: Volume: Page:1-21
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Arce J.L.¹^ORCID,Valdez G.²,Schaaf P.³,Macías-Romo M.C.¹,Vasquez-Serrano A.¹,Ramírez-Espinosa J.²

Affiliation:

1. Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria Coyoacan, Ciudad de Mexico, México

2. Unidad Académica de Ciencias de la Tierra, Universidad Autónoma de Guerrero, Guerrero, México

3. Instituto de Geofísica, UNAM, Ciudad Universitaria Coyoacan, Ciudad de Mexico, México

Funder

DGAPA-UNAM

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2024.2324301

Reference56 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. 40Ar/39Ar dating, geochemistry, and isotopic analyses of the quaternary Chichinautzin volcanic field, south of Mexico City: implications for timing, eruption rate, and distribution of volcanism

3. Geology and stratigraphy of the Mexico Basin (Mexico City), central Trans-Mexican Volcanic Belt

4. The ~ 2000 yr BP Jumento volcano, one of the youngest edifices of the Chichinautzin Volcanic Field, Central Mexico

5. A late-Quaternary monogenetic volcano field in central Mexico

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