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Proto-Andean evolution of the Eastern Cordillera of Peru
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文摘

New evidence of high-grade orogeny in the Eastern Cordillera of Peru at c. 260 Ma.

Proto-Andean margin has experienced polycyclic (Famatinian, Gondwanide) orogenesis.

Implies phases of advance and retreat in a long-lived Paleozoic accretionary orogen.

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