An Alpine-style Ordovician collision complex in the Sierra de Pie de Palo, Argentina: Record of subduction of Cuyania beneath the Famatina arc

The Caucete Group and structurally overlying Pie de Palo Complex in western Argentina are characterised by two generations of west-verging folds and thrust-related shear zones, which formed under amphibolite facies conditions. The Caucete Group is separated from the Pie de Palo Complex by the Pirqui...

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Detalles Bibliográficos
Autores principales:	van Staal, C.R., Vujovich, G.I., Currie, K.L., Naipauer, M.
Formato:	JOUR
Materias:	Collision complex Cuyania Fold nappes Subduction channel Thrusts Buildings Deformation amphibolite facies collision deformation extensional tectonics folding nappe Ordovician orogeny rifting shear zone subduction Argentina San Juan [Argentina] Sierra de Pie de Palo Sierras Pampeanas
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_01918141_v33_n3_p343_vanStaal
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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