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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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Autori principali: Claudia I. Mora, John W. Valley, Fernando Ortega-Gutiérrez
Natura: Artigo
Lingua:Inglês
Pubblicazione: Universidad Nacional Autónoma de México 2019-03-01
Serie:Revista Mexicana de Ciencias Geológicas
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Accesso online:https://rmcg.unam.mx/index.php/rmcg/article/view/1336
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