Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links

Quartzitic sandstones of the sierras Bayas Group in Sierras Septentrionales of Buenos Aires are studied. Outcrops of these deformed rocks are observed at sierras Bayas and Barker localities, where quartzitic sandstones from Precambrian units are present. These rocks are compared with similar fault b...

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Bibliographic Details
Main Authors: Massabie, Armando Carlos, Nestiero, Osvaldo E.
Language:unknown
Published: 2008
Subjects:
Online Access:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v63_n2_p163_Massabie
https://hdl.handle.net/20.500.12110/paper_00044822_v63_n2_p163_Massabie
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spelling ftunibueairesbd:paper:paper_00044822_v63_n2_p163_Massabie 2023-05-15T18:21:10+02:00 Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links Massabie, Armando Carlos Nestiero, Osvaldo E. 2008 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v63_n2_p163_Massabie https://hdl.handle.net/20.500.12110/paper_00044822_v63_n2_p163_Massabie unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v63_n2_p163_Massabie http://hdl.handle.net/20.500.12110/paper_00044822_v63_n2_p163_Massabie Breccias Fault rocks Microbreccia cohesive Sierras de Buenos Aires breccia deformation mechanism extensional tectonics fault zone faulting greenschist facies metamorphism outcrop Precambrian protolith quartzite tectonic setting Argentina Buenos Aires [Argentina] Sierras Australes Sierras Septentrionales South America 2008 ftunibueairesbd https://doi.org/20.500.12110/paper_00044822_v63_n2_p163_Massabie 2023-02-16T02:27:50Z Quartzitic sandstones of the sierras Bayas Group in Sierras Septentrionales of Buenos Aires are studied. Outcrops of these deformed rocks are observed at sierras Bayas and Barker localities, where quartzitic sandstones from Precambrian units are present. These rocks are compared with similar fault breccias in Sierras Australes of Buenos Aires, which were develop in quartzitic rocks of several Paleozoic units of this region. At both regions, fault zones are subvertical layers with acute contacts on the wall rocks. An original sedimentary protolith is recognized in textures and structures preserved in all samples of Sierras Bayas. Sedimentary textures at Sierras Australes are obliterated by penetrative deformation in greenschists facies methamorphism and also show a metaquartzitic protolith. In both analyzed regions, similar cataclastic textures are observed. All these breccias and microbreccias would be associated with a major extensional tectonic event of Jurassic - Cretaceous age, which could be related to the origin of Colorado and Salado extensional basins during the opening of the South Atlantic Ocean. Fil:Massabie, A.C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Nestiero, O.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Other/Unknown Material South Atlantic Ocean Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Argentina Wall Rocks ENVELOPE(-129.312,-129.312,52.728,52.728)
institution Open Polar
collection Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
op_collection_id ftunibueairesbd
language unknown
topic Breccias
Fault rocks
Microbreccia cohesive
Sierras de Buenos Aires
breccia
deformation mechanism
extensional tectonics
fault zone
faulting
greenschist facies
metamorphism
outcrop
Precambrian
protolith
quartzite
tectonic setting
Argentina
Buenos Aires [Argentina]
Sierras Australes
Sierras Septentrionales
South America
spellingShingle Breccias
Fault rocks
Microbreccia cohesive
Sierras de Buenos Aires
breccia
deformation mechanism
extensional tectonics
fault zone
faulting
greenschist facies
metamorphism
outcrop
Precambrian
protolith
quartzite
tectonic setting
Argentina
Buenos Aires [Argentina]
Sierras Australes
Sierras Septentrionales
South America
Massabie, Armando Carlos
Nestiero, Osvaldo E.
Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links
topic_facet Breccias
Fault rocks
Microbreccia cohesive
Sierras de Buenos Aires
breccia
deformation mechanism
extensional tectonics
fault zone
faulting
greenschist facies
metamorphism
outcrop
Precambrian
protolith
quartzite
tectonic setting
Argentina
Buenos Aires [Argentina]
Sierras Australes
Sierras Septentrionales
South America
description Quartzitic sandstones of the sierras Bayas Group in Sierras Septentrionales of Buenos Aires are studied. Outcrops of these deformed rocks are observed at sierras Bayas and Barker localities, where quartzitic sandstones from Precambrian units are present. These rocks are compared with similar fault breccias in Sierras Australes of Buenos Aires, which were develop in quartzitic rocks of several Paleozoic units of this region. At both regions, fault zones are subvertical layers with acute contacts on the wall rocks. An original sedimentary protolith is recognized in textures and structures preserved in all samples of Sierras Bayas. Sedimentary textures at Sierras Australes are obliterated by penetrative deformation in greenschists facies methamorphism and also show a metaquartzitic protolith. In both analyzed regions, similar cataclastic textures are observed. All these breccias and microbreccias would be associated with a major extensional tectonic event of Jurassic - Cretaceous age, which could be related to the origin of Colorado and Salado extensional basins during the opening of the South Atlantic Ocean. Fil:Massabie, A.C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Nestiero, O.E. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
author Massabie, Armando Carlos
Nestiero, Osvaldo E.
author_facet Massabie, Armando Carlos
Nestiero, Osvaldo E.
author_sort Massabie, Armando Carlos
title Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links
title_short Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links
title_full Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links
title_fullStr Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links
title_full_unstemmed Cohesive breccias and microbreccias in quartzites in the Buenos Aires ranges: Similitude, differences, and an approximation to their tectonic links
title_sort cohesive breccias and microbreccias in quartzites in the buenos aires ranges: similitude, differences, and an approximation to their tectonic links
publishDate 2008
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v63_n2_p163_Massabie
https://hdl.handle.net/20.500.12110/paper_00044822_v63_n2_p163_Massabie
long_lat ENVELOPE(-129.312,-129.312,52.728,52.728)
geographic Argentina
Wall Rocks
geographic_facet Argentina
Wall Rocks
genre South Atlantic Ocean
genre_facet South Atlantic Ocean
op_relation https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v63_n2_p163_Massabie
http://hdl.handle.net/20.500.12110/paper_00044822_v63_n2_p163_Massabie
op_doi https://doi.org/20.500.12110/paper_00044822_v63_n2_p163_Massabie
_version_ 1766200290498838528