Tectonic evolution of the North Patagonian Andes (41°–44° S) through recognition of syntectonic strata

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The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crustal thickness and a broad lateral development determined by a broken foreland system in the retroarc zone. This particular structural system has not been fully addressed in terms of the age and mechan...

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Detalles Bibliográficos
Autores principales:	Echaurren, A., Folguera, A., Gianni, G., Orts, D., Tassara, A., Encinas, A., Giménez, M., Valencia, V.
Formato:	JOUR
Materias:	Andean orogenesis Fold-thrust belt North Patagonia Syntectonic strata Sedimentary rocks Structural geology Tectonics Volcanic rocks Balanced cross sections Fold-thrust belts Lateral propagation Patagonia Tectonic evolution Thermomechanical model Plates (structural components) crustal thickness deformation fold and thrust belt orogeny subduction tectonic evolution thermochronology topography Andes
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00401951_v677-678_n_p99_Echaurren
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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