Evolution of the Golfo San Jorge Basin: structure and tectonic regime
Evolution of the Golfo San Jorge Basin: structure and tectonic regime. The Golfo de San Jorge Basin is a basin developed to the east of the first foothills of the Patagonian Cordillera between 44° and 48° S latitude, which has a complex geological history. Its basement was structured by a large comp...
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ftunibueairesbd:paper:paper_00044822_v72_n1_p263_Ramos 2023-05-15T18:43:19+02:00 Evolution of the Golfo San Jorge Basin: structure and tectonic regime 2014 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v72_n1_p263_Ramos https://hdl.handle.net/20.500.12110/paper_00044822_v72_n1_p263_Ramos unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v72_n1_p263_Ramos http://hdl.handle.net/20.500.12110/paper_00044822_v72_n1_p263_Ramos basin evolution extensional tectonics fold and thrust belt foreland basin plate motion subduction tectonic evolution Atlantic Ocean San Jorge Gulf 2014 ftunibueairesbd https://doi.org/20.500.12110/paper_00044822_v72_n1_p263_Ramos 2023-02-16T02:08:33Z Evolution of the Golfo San Jorge Basin: structure and tectonic regime. The Golfo de San Jorge Basin is a basin developed to the east of the first foothills of the Patagonian Cordillera between 44° and 48° S latitude, which has a complex geological history. Its basement was structured by a large compressive strain associated with a Neopaleozoic collision, followed by important extensional periods linked to the Jurassic opening of the Weddell Sea. An extensional fracturing, associated with the opening of the South Atlantic in the Late Jurassic, is superimposed in an almost orthogonal orientation. An extensional regime prevailed during the Early Cretaceous, this time produced by subduction with extension governed by the absolute motion of the South American plate. The onset of compression in the Late Cretaceous controlled the tectonic load subsidence of the continental deposits of the Chubut Group in a foreland basin. This basin, with a highly segmented basement and no confined margins also favored the existence of extensional faults with subparallel orientation to the main compressive stress during the Late Cretaceous. This system prevailed during the early Paleogene, with a conspicuous stress rotation, culminating in the Oligocene with an incipient primary extension associated with an intraplate alkali basaltic volcanism. This was associated with a decrease in the absolute displacement of the South American plate. The structure of the basin obtained the present geometry in the Neogene with the final development of the Bernárdides fold and thrust belt. © 2014, Asociacion Geologica Argentina. All rights reserved. Other/Unknown Material Weddell Sea Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Weddell Sea Weddell Argentina Chubut ENVELOPE(-62.533,-62.533,-76.100,-76.100) |
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 |
basin evolution extensional tectonics fold and thrust belt foreland basin plate motion subduction tectonic evolution Atlantic Ocean San Jorge Gulf |
spellingShingle |
basin evolution extensional tectonics fold and thrust belt foreland basin plate motion subduction tectonic evolution Atlantic Ocean San Jorge Gulf Evolution of the Golfo San Jorge Basin: structure and tectonic regime |
topic_facet |
basin evolution extensional tectonics fold and thrust belt foreland basin plate motion subduction tectonic evolution Atlantic Ocean San Jorge Gulf |
description |
Evolution of the Golfo San Jorge Basin: structure and tectonic regime. The Golfo de San Jorge Basin is a basin developed to the east of the first foothills of the Patagonian Cordillera between 44° and 48° S latitude, which has a complex geological history. Its basement was structured by a large compressive strain associated with a Neopaleozoic collision, followed by important extensional periods linked to the Jurassic opening of the Weddell Sea. An extensional fracturing, associated with the opening of the South Atlantic in the Late Jurassic, is superimposed in an almost orthogonal orientation. An extensional regime prevailed during the Early Cretaceous, this time produced by subduction with extension governed by the absolute motion of the South American plate. The onset of compression in the Late Cretaceous controlled the tectonic load subsidence of the continental deposits of the Chubut Group in a foreland basin. This basin, with a highly segmented basement and no confined margins also favored the existence of extensional faults with subparallel orientation to the main compressive stress during the Late Cretaceous. This system prevailed during the early Paleogene, with a conspicuous stress rotation, culminating in the Oligocene with an incipient primary extension associated with an intraplate alkali basaltic volcanism. This was associated with a decrease in the absolute displacement of the South American plate. The structure of the basin obtained the present geometry in the Neogene with the final development of the Bernárdides fold and thrust belt. © 2014, Asociacion Geologica Argentina. All rights reserved. |
title |
Evolution of the Golfo San Jorge Basin: structure and tectonic regime |
title_short |
Evolution of the Golfo San Jorge Basin: structure and tectonic regime |
title_full |
Evolution of the Golfo San Jorge Basin: structure and tectonic regime |
title_fullStr |
Evolution of the Golfo San Jorge Basin: structure and tectonic regime |
title_full_unstemmed |
Evolution of the Golfo San Jorge Basin: structure and tectonic regime |
title_sort |
evolution of the golfo san jorge basin: structure and tectonic regime |
publishDate |
2014 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v72_n1_p263_Ramos https://hdl.handle.net/20.500.12110/paper_00044822_v72_n1_p263_Ramos |
long_lat |
ENVELOPE(-62.533,-62.533,-76.100,-76.100) |
geographic |
Weddell Sea Weddell Argentina Chubut |
geographic_facet |
Weddell Sea Weddell Argentina Chubut |
genre |
Weddell Sea |
genre_facet |
Weddell Sea |
op_relation |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v72_n1_p263_Ramos http://hdl.handle.net/20.500.12110/paper_00044822_v72_n1_p263_Ramos |
op_doi |
https://doi.org/20.500.12110/paper_00044822_v72_n1_p263_Ramos |
_version_ |
1766233642522116096 |