Age constraints on the tectonic evolution and provenance of the Pie de Palo Complex, Cuyania composite terrane and the Famatinian orogeny in the Sierra de Pie de Palo, San Juan, Argentina

New U-Pb age determinations confirm earlier interpretations that the strongly deformed and metamorphosed mafic and intermediate igneous rocks of the Pie de Palo Complex represent a Mesoproterozoic fragment of suprasubduction zone oceanic crust. A gabbroic pegmatite, interpreted to have formed during...

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Detalles Bibliográficos
Autor principal:	Vujovich, Graciela Irene
Publicado:	2004
Materias:	Back-arc Cuyania Grenville Island arc Ophiolite
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_1342937X_v7_n4_p1041_Vujovich http://hdl.handle.net/20.500.12110/paper_1342937X_v7_n4_p1041_Vujovich
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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