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Provenance model of the Cenozoic siliciclastic sediments from the western Central Andes (16-21°S): implications for Eocene to Miocene evolution of the Andes408

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Provenance model of the Cenozoic siliciclastic sediments from the western Central Andes (16-21°S): implications for Eocene to Miocene evolution of the Andes385106100

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