High-Temperature Metamorphic Garnets from Grenvillian Granulites of Southwestern Oaxacan Complex (Southern Mexico): Petrology, Geochemistry, Geothermobarometry, and Tectonic Implications

High-Temperature Metamorphic Garnets from Grenvillian Granulites of Southwestern Oaxacan Complex (Southern Mexico): Petrology, Geochemistry, Geothermobarometry, and Tectonic Implications

The basement of eastern Mexico comprises Grenvillian-age granulite-facies metamorphic rocks. The Oaxacan Complex represents the largest outcrop belt of this basement in Mexico. In this work, southwestern Oaxacan Complex garnets are studied from a petrographical, geochemical, and geothermobarometrica...

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Bibliographic Details
Main Authors: Laura Culí, Jesús Solé, Marc Campeny, Jeffry A. G. Oalmann
Format: Article
Language:English
Published: MDPI AG 2021-07-01
Series:Minerals
Subjects:
Grenvillian orogeny
Oaxacan Complex
garnet main end members
minor and trace elements
garnet geothermobarometry
structural levels
Online Access:https://www.mdpi.com/2075-163X/11/8/805

Internet

https://www.mdpi.com/2075-163X/11/8/805

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