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Multiple metamorphic stages within an eclogite-facies terrane (Sesia Zone, Western Alps) revealed by Th-U-Pb petrochronology

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Authors

Regis, Daniele
Rubatto, Daniela
Darling, James
Cenki-Tok, Bénédicte
Zucali, Michele
Engi, Martin

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Oxford University Press

Abstract

Convergent plate margins typically experience a transition from subduction to collision dynamics as massive continental blocks enter the subduction channel. Studies of high-pressure rocks indicate that tectonic fragments are rapidly exhumed from eclogite

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Source

Journal of Petrology

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Restricted until

2037-12-31