Sr-Nb-Pb isotopes in Miocene porphyry copper deposits from Precordillera of Mendoza, Argentina

The Paramillos de Uspallata mining district is located in the southern part of the Precordillera of Mendoza Province (69°05’-69°07’W; 32°24’-32°31’S), in the Cenozoic flat-slab segment (27-33°S) of Chile and Argentina. The district includes the porphyry copper deposits Paramillos Norte, Paramillos C...

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Detalles Bibliográficos
Autores principales: Carrasquero, Silvia Irene, Rubinstein, Nora A., Fontignie, Denis, Chiaradia, Massimo
Formato: Articulo Comunicacion
Lenguaje:Inglés
Publicado: 2013
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/74767
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Sumario:The Paramillos de Uspallata mining district is located in the southern part of the Precordillera of Mendoza Province (69°05’-69°07’W; 32°24’-32°31’S), in the Cenozoic flat-slab segment (27-33°S) of Chile and Argentina. The district includes the porphyry copper deposits Paramillos Norte, Paramillos Centro and Paramillos Sur. These ore deposits are genetically linked to the Miocene volcanism with an adakite-like signature.