Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup

From Lower Jurassic to Lower Cretaceous, several intraplate compression events affected discrete sectors of Central Patagonia, under a general context of crustal extension associated with Gondwana breakup. This was demonstrated by means of 2D and 3D seismic and borehole data, which show partial inve...

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Main Authors: Navarrete, C., Gianni, G., Echaurren, A., Kingler, F.L., Folguera, A.
Format: Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://hdl.handle.net/20.500.12110/paper_02643707_v102_n_p185_Navarrete
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spelling ftunibueairesbd:todo:paper_02643707_v102_n_p185_Navarrete 2023-10-29T02:40:45+01:00 Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup Navarrete, C. Gianni, G. Echaurren, A. Kingler, F.L. Folguera, A. https://hdl.handle.net/20.500.12110/paper_02643707_v102_n_p185_Navarrete unknown http://hdl.handle.net/20.500.12110/paper_02643707_v102_n_p185_Navarrete info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Intraplate compression Jurassic to Lower Cretaceous inversion Karoo large igneous province Supercontinent break-up JOUR ftunibueairesbd https://doi.org/20.500.12110/paper_02643707_v102_n_p185_Navarrete 2023-10-05T01:15:07Z From Lower Jurassic to Lower Cretaceous, several intraplate compression events affected discrete sectors of Central Patagonia, under a general context of crustal extension associated with Gondwana breakup. This was demonstrated by means of 2D and 3D seismic and borehole data, which show partial inversion of Lower and Middle Jurassic extensional structures of the Chubut and Cañadón Asfalto basins, during the earliest stages of breakup. A comparison with surrounding areas in Patagonia, where similar Jurassic intraplate compression was described, allowed the discrimination of three discrete pulses of subtle compression (C1: ∼188–185 Ma; C2: ∼170–163; C3: ∼157–136? Ma). Interestingly, episodic intraplate compressional events are closely followed by high flux magmatic events linked to the westward expansion of the Karoo-Ferrar thermal anomaly, which impacted on the lithosphere of southwest Gondwana in Lower Jurassic. In addition, we determined the approximate direction of the main compressive strain (σ1) compatible with other Jurassic intraplate belts of South America. These observations led us to propose a linkage between a thermo mechanically weakened continental crust due to LIPs activity, changes in plate motions and ridge-push forces generated by the opening of the Weddell Sea, in order to explain intraplate shortening, interrupted while Karoo LIPs magmatic invigoration took place. © 2016 Elsevier Ltd Fil:Gianni, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Folguera, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Journal/Newspaper Weddell Sea Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
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 Intraplate compression
Jurassic to Lower Cretaceous inversion
Karoo large igneous province
Supercontinent break-up
spellingShingle Intraplate compression
Jurassic to Lower Cretaceous inversion
Karoo large igneous province
Supercontinent break-up
Navarrete, C.
Gianni, G.
Echaurren, A.
Kingler, F.L.
Folguera, A.
Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup
topic_facet Intraplate compression
Jurassic to Lower Cretaceous inversion
Karoo large igneous province
Supercontinent break-up
description From Lower Jurassic to Lower Cretaceous, several intraplate compression events affected discrete sectors of Central Patagonia, under a general context of crustal extension associated with Gondwana breakup. This was demonstrated by means of 2D and 3D seismic and borehole data, which show partial inversion of Lower and Middle Jurassic extensional structures of the Chubut and Cañadón Asfalto basins, during the earliest stages of breakup. A comparison with surrounding areas in Patagonia, where similar Jurassic intraplate compression was described, allowed the discrimination of three discrete pulses of subtle compression (C1: ∼188–185 Ma; C2: ∼170–163; C3: ∼157–136? Ma). Interestingly, episodic intraplate compressional events are closely followed by high flux magmatic events linked to the westward expansion of the Karoo-Ferrar thermal anomaly, which impacted on the lithosphere of southwest Gondwana in Lower Jurassic. In addition, we determined the approximate direction of the main compressive strain (σ1) compatible with other Jurassic intraplate belts of South America. These observations led us to propose a linkage between a thermo mechanically weakened continental crust due to LIPs activity, changes in plate motions and ridge-push forces generated by the opening of the Weddell Sea, in order to explain intraplate shortening, interrupted while Karoo LIPs magmatic invigoration took place. © 2016 Elsevier Ltd Fil:Gianni, G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Folguera, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina.
format Journal/Newspaper
author Navarrete, C.
Gianni, G.
Echaurren, A.
Kingler, F.L.
Folguera, A.
author_facet Navarrete, C.
Gianni, G.
Echaurren, A.
Kingler, F.L.
Folguera, A.
author_sort Navarrete, C.
title Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup
title_short Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup
title_full Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup
title_fullStr Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup
title_full_unstemmed Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup
title_sort episodic jurassic to lower cretaceous intraplate compression in central patagonia during gondwana breakup
url https://hdl.handle.net/20.500.12110/paper_02643707_v102_n_p185_Navarrete
genre Weddell Sea
genre_facet Weddell Sea
op_relation http://hdl.handle.net/20.500.12110/paper_02643707_v102_n_p185_Navarrete
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/2.5/ar
op_doi https://doi.org/20.500.12110/paper_02643707_v102_n_p185_Navarrete
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