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The petrogenesis of Early–Middle Jurassic magmatism in southern and central Mexico and its role during the break-up of Western Pangaea

Published online by Cambridge University Press:  21 February 2022

Mattia Parolari Open the ORCID record for Mattia Parolari [Opens in a new window] ,
Michelangelo Martini ,
Arturo Gómez-Tuena ,
Fernando Ortega-Gutiérrez ,
Carlos Errázuriz-Henao  and
José G. Cavazos-Tovar
Mattia Parolari*
Affiliation:
Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria 04510, Mexico City, Mexico
Michelangelo Martini
Affiliation:
Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria 04510, Mexico City, Mexico
Arturo Gómez-Tuena
Affiliation:
Centro de Geociencias, Universidad Nacional Autónoma de México, Querétaro76230, Mexico
Fernando Ortega-Gutiérrez
Affiliation:
Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria 04510, Mexico City, Mexico
Carlos Errázuriz-Henao
Affiliation:
Centro de Geociencias, Universidad Nacional Autónoma de México, Querétaro76230, Mexico
José G. Cavazos-Tovar
Affiliation:
Centro de Geociencias, Universidad Nacional Autónoma de México, Querétaro76230, Mexico
*
Author for correspondence: Mattia Parolari, Email: [email protected]
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Abstract

Central and southern Mexico represents a strategic place to understand the dynamics of Pangaea break-up and its influences on the evolution of the Pacific margin of North America. Lower–Middle Jurassic volcano-sedimentary successions, and scarce magmatic rocks, crop out discontinuously across this region and have been interpreted either as a vestige of a continental arc or as several deposits of syn-rift magmatism. At present, their origin is controversial. Available geochemical data on these igneous rocks suggest that they represent almost pure crustal melts produced in a rift environment rather than in an arc. In fact, the studied rocks exhibit the high silica contents and moderate to strong peraluminous character typical of sediment melts. The enriched isotopic composition (high 86Sr/87Sr and low 143Nd/144Nd) and the age distributions of inherited zircon grains readily identify the widespread Upper Triassic metasedimentary sequences presently exposed in southwestern and central Mexico as the most likely crustal source of these Jurassic igneous rocks. Accordingly, we argue that these Early–Middle Jurassic magmas originated in a syn-rift igneous province associated with extensional-driven crustal attenuation in the context of Pangaea fragmentation. Our findings also constrain post-Pangaea subduction initiation to be younger than Middle Jurassic time in central and southern Mexico.

Keywords

Mexican continental marginNazas igneous provincesyn-rift Jurassic magmatismPangaea break-upsubduction initiation
Type
Original Article
Information
Geological Magazine , Volume 159 , Issue 6 , June 2022 , pp. 873 - 892
Copyright
© The Author(s), 2022. Published by Cambridge University Press

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