Detrital zircon analysis from the Neoproterozoic-Cambrian sedimentary cover (Cuyania terrane), Sierra de Pie de Palo, Argentina: Evidence of a rift and passive margin system?

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Metamorphic basement and its Neoproterozoic to Cambrian cover exposed in the Sierra de Pie de Palo, a basement block of the Sierras Pampeanas in Argentina, lie within the Cuyania terrane. Detrital zircon analysis of the cover sequence which includes, in ascending order, the El Quemado, La Paz, El De...

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Detalles Bibliográficos
Autores principales:	Naipauer, M., Vujovich, G.I., Cingolani, C.A., McClelland, W.C.
Formato:	JOUR
Materias:	Cuyania terrane Detrital zircon Sierra de Pie de Palo U/Pb (LA-ICP-MS) Western Argentina basement rock Cambrian detrital deposit igneous rock Laurentia passive margin Proterozoic provenance rifting sedimentary sequence sedimentation source rock uranium-lead dating zircon Argentina Precordillera San Juan [Argentina] Sierras Pampeanas Typha domingensis
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_08959811_v29_n2_p306_Naipauer
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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