Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza

The Aconcagua and Malargüe fold and thrust belts developed in the Cordillera Principal, which between 32° 34° and 34°-36° S latitude respectively, show a complex interaction between the sedimentary cover and the basement as a result of the existence of Triassic-Jurassic rift-related normal faults of...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Giambiagi, L., Alvarez, P.P., Bechis, F., Tunik, M.
Formato:	JOUR
Materias:	Aconcagua Andean deformation Fold and thrust belt Jurassic Malargúe Neuquén Basin chronology deformation mechanism fault fold and thrust belt inversion tectonics normal fault rift zone tectonic evolution thin skinned tectonics Triassic Andes Argentina Malargue Mendoza Neuquen South America
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p662_Giambiagi
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	todo:paper_00044822_v60_n4_p662_Giambiagi
record_format	dspace
spelling	todo:paper_00044822_v60_n4_p662_Giambiagi2023-10-03T13:58:08Z Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza Giambiagi, L. Alvarez, P.P. Bechis, F. Tunik, M. Aconcagua Andean deformation Fold and thrust belt Jurassic Malargúe Neuquén Basin chronology deformation mechanism fault fold and thrust belt inversion tectonics Jurassic normal fault rift zone tectonic evolution thin skinned tectonics Triassic Aconcagua Andes Argentina Malargue Mendoza Neuquen South America The Aconcagua and Malargüe fold and thrust belts developed in the Cordillera Principal, which between 32° 34° and 34°-36° S latitude respectively, show a complex interaction between the sedimentary cover and the basement as a result of the existence of Triassic-Jurassic rift-related normal faults of the northern part of the Neuquén basin. Structural studies, together with chronological analysis of the deformation in the thin-skinned and thick-skinned zones, indicate that the evolution of both belts was controlled by the presence of NNW-trending border faults of the Atuel, Nieves Negras - Alvarado and Yeguas Muertas depocentres of the Neuquén basin. In this study we analyze three possible mechanisms of interaction between the thin-skinned and thick-skinned deformation. For the Aconcagua FTB, we propose that the pre-existing normal faults controlled the location of ramps within the basement. For the southernmost part of the Aconcagua FTB and the northern part of the Malargüe FTB we propose a mechanism of tectonic inversion of rift-related faults, together with short-cut faults, which propagated into the sedimentary cover generation the thin-skinned deformational area. © 2005 Asociación Geológica Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p662_Giambiagi
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Aconcagua Andean deformation Fold and thrust belt Jurassic Malargúe Neuquén Basin chronology deformation mechanism fault fold and thrust belt inversion tectonics Jurassic normal fault rift zone tectonic evolution thin skinned tectonics Triassic Aconcagua Andes Argentina Malargue Mendoza Neuquen South America
spellingShingle	Aconcagua Andean deformation Fold and thrust belt Jurassic Malargúe Neuquén Basin chronology deformation mechanism fault fold and thrust belt inversion tectonics Jurassic normal fault rift zone tectonic evolution thin skinned tectonics Triassic Aconcagua Andes Argentina Malargue Mendoza Neuquen South America Giambiagi, L. Alvarez, P.P. Bechis, F. Tunik, M. Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
topic_facet	Aconcagua Andean deformation Fold and thrust belt Jurassic Malargúe Neuquén Basin chronology deformation mechanism fault fold and thrust belt inversion tectonics Jurassic normal fault rift zone tectonic evolution thin skinned tectonics Triassic Aconcagua Andes Argentina Malargue Mendoza Neuquen South America
description	The Aconcagua and Malargüe fold and thrust belts developed in the Cordillera Principal, which between 32° 34° and 34°-36° S latitude respectively, show a complex interaction between the sedimentary cover and the basement as a result of the existence of Triassic-Jurassic rift-related normal faults of the northern part of the Neuquén basin. Structural studies, together with chronological analysis of the deformation in the thin-skinned and thick-skinned zones, indicate that the evolution of both belts was controlled by the presence of NNW-trending border faults of the Atuel, Nieves Negras - Alvarado and Yeguas Muertas depocentres of the Neuquén basin. In this study we analyze three possible mechanisms of interaction between the thin-skinned and thick-skinned deformation. For the Aconcagua FTB, we propose that the pre-existing normal faults controlled the location of ramps within the basement. For the southernmost part of the Aconcagua FTB and the northern part of the Malargüe FTB we propose a mechanism of tectonic inversion of rift-related faults, together with short-cut faults, which propagated into the sedimentary cover generation the thin-skinned deformational area. © 2005 Asociación Geológica Argentina.
format	JOUR
author	Giambiagi, L. Alvarez, P.P. Bechis, F. Tunik, M.
author_facet	Giambiagi, L. Alvarez, P.P. Bechis, F. Tunik, M.
author_sort	Giambiagi, L.
title	Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
title_short	Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
title_full	Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
title_fullStr	Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
title_full_unstemmed	Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
title_sort	lnfluence of the triassic-jurassic rift structures on the deformation style of the aconcagua and maragüe fold and thrust belts, mendoza
url	http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p662_Giambiagi
work_keys_str_mv	AT giambiagil lnfluenceofthetriassicjurassicriftstructuresonthedeformationstyleoftheaconcaguaandmaraguefoldandthrustbeltsmendoza AT alvarezpp lnfluenceofthetriassicjurassicriftstructuresonthedeformationstyleoftheaconcaguaandmaraguefoldandthrustbeltsmendoza AT bechisf lnfluenceofthetriassicjurassicriftstructuresonthedeformationstyleoftheaconcaguaandmaraguefoldandthrustbeltsmendoza AT tunikm lnfluenceofthetriassicjurassicriftstructuresonthedeformationstyleoftheaconcaguaandmaraguefoldandthrustbeltsmendoza
_version_	1807316675553394688

Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza

Ejemplares similares