The temperature and pressure conditions of Grenville-age granulite facies metamorphism of the Oaxacan Complex, southern Mexico

The temperatura, pressure and fluid conditions at peak of granulite facies metamorphism have been determined for charnockites, marbles and quartzofeldspathic gneises in the Grenville-age Oaxaca Complex, southern Mexico… In order to continue, download the full paper in PDF.

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Bibliographic Details
Main Authors: Claudia I. Mora, John W. Valley, Fernando Ortega-Gutiérrez
Format: Article
Language:English
Published: Universidad Nacional Autónoma de México 2019-03-01
Series:Revista Mexicana de Ciencias Geológicas
Subjects:
Online Access:https://rmcg.unam.mx/index.php/rmcg/article/view/1336
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