Stratigraphy and structure of the río Borbollón area, Mendoza

Results of a detailed geologic survey of the Río Borbollón area, located in the Cordillera Principal of the province of Mendoza are presented. The stratigraphic record of the area corresponds to a Jurassic-early Cretaceous sedimentary succession, the products of Neogene igneous activity and Quaterna...

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Autores principales:	Mescua, José Francisco, Ramos, Victor Alberto
Publicado:	2009
Materias:	Andes Argentina Jurassic deposits Malargüe fold and thrust belt Neuquén basin Structure crustal shortening fold and thrust belt geological record geological survey Jurassic-Cretaceous boundary orogenic belt sedimentary sequence stratigraphy structural geology Malargue Mendoza Neuquen Basin
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v65_n1_p111_Mescua http://hdl.handle.net/20.500.12110/paper_00044822_v65_n1_p111_Mescua
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	paper:paper_00044822_v65_n1_p111_Mescua
record_format	dspace
spelling	paper:paper_00044822_v65_n1_p111_Mescua2023-06-08T14:26:15Z Stratigraphy and structure of the río Borbollón area, Mendoza Mescua, José Francisco Ramos, Victor Alberto Andes Argentina Jurassic deposits Malargüe fold and thrust belt Neuquén basin Structure crustal shortening fold and thrust belt geological record geological survey Jurassic-Cretaceous boundary orogenic belt sedimentary sequence stratigraphy structural geology Andes Argentina Malargue Mendoza Neuquen Basin Results of a detailed geologic survey of the Río Borbollón area, located in the Cordillera Principal of the province of Mendoza are presented. The stratigraphic record of the area corresponds to a Jurassic-early Cretaceous sedimentary succession, the products of Neogene igneous activity and Quaternary deposits. The Tres Esquinas and La Manga Formations of Jurassic age were recognized for the first time in the study area. The main structural features of the area are described and interpreted based on the obtained data and previous works. A balanced structural cross section of the Malargüe fold and thrust belt at 34°15'S depicts the structural style and the amount of orogenic shortening in this region of the Andes. Fil:Mescua, J.F. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Ramos, V.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2009 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v65_n1_p111_Mescua http://hdl.handle.net/20.500.12110/paper_00044822_v65_n1_p111_Mescua
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Andes Argentina Jurassic deposits Malargüe fold and thrust belt Neuquén basin Structure crustal shortening fold and thrust belt geological record geological survey Jurassic-Cretaceous boundary orogenic belt sedimentary sequence stratigraphy structural geology Andes Argentina Malargue Mendoza Neuquen Basin
spellingShingle	Andes Argentina Jurassic deposits Malargüe fold and thrust belt Neuquén basin Structure crustal shortening fold and thrust belt geological record geological survey Jurassic-Cretaceous boundary orogenic belt sedimentary sequence stratigraphy structural geology Andes Argentina Malargue Mendoza Neuquen Basin Mescua, José Francisco Ramos, Victor Alberto Stratigraphy and structure of the río Borbollón area, Mendoza
topic_facet	Andes Argentina Jurassic deposits Malargüe fold and thrust belt Neuquén basin Structure crustal shortening fold and thrust belt geological record geological survey Jurassic-Cretaceous boundary orogenic belt sedimentary sequence stratigraphy structural geology Andes Argentina Malargue Mendoza Neuquen Basin
description	Results of a detailed geologic survey of the Río Borbollón area, located in the Cordillera Principal of the province of Mendoza are presented. The stratigraphic record of the area corresponds to a Jurassic-early Cretaceous sedimentary succession, the products of Neogene igneous activity and Quaternary deposits. The Tres Esquinas and La Manga Formations of Jurassic age were recognized for the first time in the study area. The main structural features of the area are described and interpreted based on the obtained data and previous works. A balanced structural cross section of the Malargüe fold and thrust belt at 34°15'S depicts the structural style and the amount of orogenic shortening in this region of the Andes.
author	Mescua, José Francisco Ramos, Victor Alberto
author_facet	Mescua, José Francisco Ramos, Victor Alberto
author_sort	Mescua, José Francisco
title	Stratigraphy and structure of the río Borbollón area, Mendoza
title_short	Stratigraphy and structure of the río Borbollón area, Mendoza
title_full	Stratigraphy and structure of the río Borbollón area, Mendoza
title_fullStr	Stratigraphy and structure of the río Borbollón area, Mendoza
title_full_unstemmed	Stratigraphy and structure of the río Borbollón area, Mendoza
title_sort	stratigraphy and structure of the río borbollón area, mendoza
publishDate	2009
url	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v65_n1_p111_Mescua http://hdl.handle.net/20.500.12110/paper_00044822_v65_n1_p111_Mescua
work_keys_str_mv	AT mescuajosefrancisco stratigraphyandstructureoftherioborbollonareamendoza AT ramosvictoralberto stratigraphyandstructureoftherioborbollonareamendoza
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Stratigraphy and structure of the río Borbollón area, Mendoza

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