Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)

This article describes the volcanic and sedimentary stratigraphy and their associated processes with the Andean deformation during the Late Cretaceous to Late Pliocene. The studied area is located between the Atuel and Barrancas rivers and the Main Cordillera, in southern Mendoza, Argentina. Three t...

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Detalles Bibliográficos
Publicado:	2011
Materias:	Argentina Cenozoic Southern Mendoza Stratigraphy Volcanism deformation Miocene Oligocene Pliocene sedimentary sequence sequence stratigraphy tectonics volcanism Atuel River Barrancas River Mendoza Diaguita
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v38_n1_p198_Combina http://hdl.handle.net/20.500.12110/paper_07187092_v38_n1_p198_Combina
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	paper:paper_07187092_v38_n1_p198_Combina
record_format	dspace
spelling	paper:paper_07187092_v38_n1_p198_Combina2023-06-08T15:43:11Z Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W) Argentina Cenozoic Southern Mendoza Stratigraphy Volcanism deformation Miocene Oligocene Pliocene sedimentary sequence sequence stratigraphy tectonics volcanism Argentina Atuel River Barrancas River Mendoza Diaguita This article describes the volcanic and sedimentary stratigraphy and their associated processes with the Andean deformation during the Late Cretaceous to Late Pliocene. The studied area is located between the Atuel and Barrancas rivers and the Main Cordillera, in southern Mendoza, Argentina. Three tectovolcanosedimentary cycles limited by regional discordances (Inca, Quechua, Pehuenche and Diaguita) are proposed. The first comprises Upper Oligocene to Upper Miocene volcanic and sedimentary units (Roca and Pircala-Coihueco formations and the Volcanic Cycle Molle). The second extends from the Late Oligocene to Late Miocene (Agua de la Piedra Formation and the Huincán Andesites volcanic cycle). Finally, the third cycle ranges from the Late Miocene to Pliocene (Butaló, Pincheiras, Loma Fiera and Rio Diamante formations and La Brea Andesites). 2011 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v38_n1_p198_Combina http://hdl.handle.net/20.500.12110/paper_07187092_v38_n1_p198_Combina
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Argentina Cenozoic Southern Mendoza Stratigraphy Volcanism deformation Miocene Oligocene Pliocene sedimentary sequence sequence stratigraphy tectonics volcanism Argentina Atuel River Barrancas River Mendoza Diaguita
spellingShingle	Argentina Cenozoic Southern Mendoza Stratigraphy Volcanism deformation Miocene Oligocene Pliocene sedimentary sequence sequence stratigraphy tectonics volcanism Argentina Atuel River Barrancas River Mendoza Diaguita Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)
topic_facet	Argentina Cenozoic Southern Mendoza Stratigraphy Volcanism deformation Miocene Oligocene Pliocene sedimentary sequence sequence stratigraphy tectonics volcanism Argentina Atuel River Barrancas River Mendoza Diaguita
description	This article describes the volcanic and sedimentary stratigraphy and their associated processes with the Andean deformation during the Late Cretaceous to Late Pliocene. The studied area is located between the Atuel and Barrancas rivers and the Main Cordillera, in southern Mendoza, Argentina. Three tectovolcanosedimentary cycles limited by regional discordances (Inca, Quechua, Pehuenche and Diaguita) are proposed. The first comprises Upper Oligocene to Upper Miocene volcanic and sedimentary units (Roca and Pircala-Coihueco formations and the Volcanic Cycle Molle). The second extends from the Late Oligocene to Late Miocene (Agua de la Piedra Formation and the Huincán Andesites volcanic cycle). Finally, the third cycle ranges from the Late Miocene to Pliocene (Butaló, Pincheiras, Loma Fiera and Rio Diamante formations and La Brea Andesites).
title	Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)
title_short	Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)
title_full	Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)
title_fullStr	Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)
title_full_unstemmed	Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)
title_sort	cenozoic tectonic, volcanic and sedimentary cycles in southern mendoza province, argentina (35°-37°s y 69°30'w)
publishDate	2011
url	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_07187092_v38_n1_p198_Combina http://hdl.handle.net/20.500.12110/paper_07187092_v38_n1_p198_Combina
_version_	1768544414980898816

Cenozoic tectonic, volcanic and sedimentary cycles in southern Mendoza province, Argentina (35°-37°S y 69°30'W)

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