Tectonic and tectosedimentary characteristics of the Rincón Blanco halfgraben: A synthesis

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The Gondwana margin contained some Triassic basins that together constitute a regionally northwest-trending extensional system. The Cuyana rift Basin is internally composed of a family of hemigrabens filled with thick piles of sedimentary clastic and epiclastic rocks that can reach more than three t...

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Detalles Bibliográficos
Autores principales:	Barredo, S., Ramos, V.A.
Formato:	JOUR
Materias:	Normal fault growth Rift Rincón Blanco hemigraben Sedimentary controls Stratigraphy basin evolution displacement extensional tectonics fault geometry graben normal fault rift zone structural control synsedimentary tectonics tectonic evolution tectonic setting tectonostratigraphy Argentina Cuyana Basin Cuyana
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v66_n1-2_p133_Barredo
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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