Mid-Tertiary cooling ages in the Precambrian Oaxacan Complex of southern Mexico: indication of exhumation and inland arc migration

In southern Mexico, the ~1 Ga Oaxacan Complex is in fault contact with the Mesozoic–CenozoicChatino terrane. 40Ar/39Ar dating of minerals from hornblende gneiss and quartz monzonitic gneiss inthe southern Oaxacan Complex collected, 10 km and 1 km north of the Oaxaca–Xolapa boundary,yielded the follo...

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Detalhes bibliográficos
Publicado no:Revista Mexicana de Ciencias Geológicas
Main Authors: Amabel Ortega Rivera, Carlos Heinrich Schulze, James K. W. Lee, John Duncan Keppie, Fernando Ortega Gutiérrez
Formato: Artigo
Idioma:Inglês
Publicado em: Universidad Nacional Autónoma de México 2004
Assuntos:
Ciencias de la Tierra
Tertiary
Precambrian
cooling ages
arc magmatism
Oaxacan Complex
Acesso em linha:https://www.redalyc.org/articulo.oa?id=57221201
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