Karakoram fault zone rocks cool in two phases

The Karakoram fault zone of Ladakh, India, is a major strike-slip boundary along which the tectonic evolution of Tibet has been accommodated. In this paper 40Ar/39Ar isotopic age data are integrated with structural and metamorphic data to infer an exhumation history for granites and low- to intermed...

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Détails bibliographiques
Auteurs principaux: Dunlap, W, Weinberg, R, Searle, M
Format: Journal article
Langue:English
Publié: 1998