Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation
Group of microstructures present in the Ordovician Yerba Loca and Los Sombreros Formations (cropping out in the vicinity of Road 150, between cuesta del Viento and Los Túneles), are described and interpreted. Cleavage, joints and fractures, shear zones, planar and sigmoid (en echelon) veins and kink...
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Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v66_n1-2_p94_SellesMartinez http://hdl.handle.net/20.500.12110/paper_00044822_v66_n1-2_p94_SellesMartinez |
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paper:paper_00044822_v66_n1-2_p94_SellesMartinez2023-06-08T14:26:24Z Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation Selles Martinez, José Azcurra, Diego Jáchal River Minor structures Palaeozoic Precordillera Yerba Loca Formation deformation displacement geological structure headwater microstructure Ordovician Paleozoic recrystallization shear zone stress field Argentina Jachal River San Juan [Argentina] Croton ovalifolius Group of microstructures present in the Ordovician Yerba Loca and Los Sombreros Formations (cropping out in the vicinity of Road 150, between cuesta del Viento and Los Túneles), are described and interpreted. Cleavage, joints and fractures, shear zones, planar and sigmoid (en echelon) veins and kink bands are most common among them. Folded and domino faulted quartz veins, resulting from pressure solution contraction during formation of axial plane cleavage, are an outstanding feature and allowed calculation of contraction associated to cleavage development. The assemblage of minor structures shows coherency with the major structures hosting them and evidences a systematic displacement and stacking of rock masses from west to east. They also show the important participation of pressure solution and re-crystallization processes during deformation, along with progressive deformation due to rotation of local structures in the regional stress field. Fil:Sellés-Martínez, J. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Azcurra, D. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2010 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v66_n1-2_p94_SellesMartinez http://hdl.handle.net/20.500.12110/paper_00044822_v66_n1-2_p94_SellesMartinez |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Jáchal River Minor structures Palaeozoic Precordillera Yerba Loca Formation deformation displacement geological structure headwater microstructure Ordovician Paleozoic recrystallization shear zone stress field Argentina Jachal River San Juan [Argentina] Croton ovalifolius |
spellingShingle |
Jáchal River Minor structures Palaeozoic Precordillera Yerba Loca Formation deformation displacement geological structure headwater microstructure Ordovician Paleozoic recrystallization shear zone stress field Argentina Jachal River San Juan [Argentina] Croton ovalifolius Selles Martinez, José Azcurra, Diego Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation |
topic_facet |
Jáchal River Minor structures Palaeozoic Precordillera Yerba Loca Formation deformation displacement geological structure headwater microstructure Ordovician Paleozoic recrystallization shear zone stress field Argentina Jachal River San Juan [Argentina] Croton ovalifolius |
description |
Group of microstructures present in the Ordovician Yerba Loca and Los Sombreros Formations (cropping out in the vicinity of Road 150, between cuesta del Viento and Los Túneles), are described and interpreted. Cleavage, joints and fractures, shear zones, planar and sigmoid (en echelon) veins and kink bands are most common among them. Folded and domino faulted quartz veins, resulting from pressure solution contraction during formation of axial plane cleavage, are an outstanding feature and allowed calculation of contraction associated to cleavage development. The assemblage of minor structures shows coherency with the major structures hosting them and evidences a systematic displacement and stacking of rock masses from west to east. They also show the important participation of pressure solution and re-crystallization processes during deformation, along with progressive deformation due to rotation of local structures in the regional stress field. |
author |
Selles Martinez, José Azcurra, Diego |
author_facet |
Selles Martinez, José Azcurra, Diego |
author_sort |
Selles Martinez, José |
title |
Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation |
title_short |
Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation |
title_full |
Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation |
title_fullStr |
Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation |
title_full_unstemmed |
Lower Paleozoic microestructures in the headwaters of Río Jachal, San Juan Province: Their description and interpretation |
title_sort |
lower paleozoic microestructures in the headwaters of río jachal, san juan province: their description and interpretation |
publishDate |
2010 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v66_n1-2_p94_SellesMartinez http://hdl.handle.net/20.500.12110/paper_00044822_v66_n1-2_p94_SellesMartinez |
work_keys_str_mv |
AT sellesmartinezjose lowerpaleozoicmicroestructuresintheheadwatersofriojachalsanjuanprovincetheirdescriptionandinterpretation AT azcurradiego lowerpaleozoicmicroestructuresintheheadwatersofriojachalsanjuanprovincetheirdescriptionandinterpretation |
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1768543971162718208 |