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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Published in:Journal of Geodynamics
Main Authors: Navarrete Granzotto, César Rodrigo, Gianni, Guido Martin, Echaurren Gonzalez, Andres, Lince Klinger, Federico Gustavo, Folguera Telichevsky, Andres
Format: Article in Journal/Newspaper
Language:English
Published: Pergamon-Elsevier Science Ltd
Subjects:
Online Access:http://hdl.handle.net/11336/46796
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author Navarrete Granzotto, César Rodrigo
Gianni, Guido Martin
Echaurren Gonzalez, Andres
Lince Klinger, Federico Gustavo
Folguera Telichevsky, Andres
author_facet Navarrete Granzotto, César Rodrigo
Gianni, Guido Martin
Echaurren Gonzalez, Andres
Lince Klinger, Federico Gustavo
Folguera Telichevsky, Andres
author_sort Navarrete Granzotto, César Rodrigo
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_start_page 185
container_title Journal of Geodynamics
container_volume 102
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 Ca ?nadón Asfalto basins, during the earliest stages of breakup. A comparison with surrounding areas in Patagonia, where similar Juras-sic 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 expan-sion 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 (1) compatible with other Jurassic intraplate belts of South America. These observations led us to pro-pose 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. Fil: Navarrete Granzotto, César Rodrigo. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Gianni, Guido Martin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Echaurren Gonzalez, Andres. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación ...
format Article in Journal/Newspaper
genre Weddell Sea
genre_facet Weddell Sea
geographic Weddell Sea
Patagonia
San Juan
Weddell
Argentina
Chubut
Sion
Gonzalez
Pablo
Guido
Navarrete
geographic_facet Weddell Sea
Patagonia
San Juan
Weddell
Argentina
Chubut
Sion
Gonzalez
Pablo
Guido
Navarrete
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op_doi https://doi.org/10.1016/j.jog.2016.10.001
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/46796 2025-01-17T01:16:46+00:00 Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup Navarrete Granzotto, César Rodrigo Gianni, Guido Martin Echaurren Gonzalez, Andres Lince Klinger, Federico Gustavo Folguera Telichevsky, Andres application/pdf http://hdl.handle.net/11336/46796 eng eng Pergamon-Elsevier Science Ltd info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jog.2016.10.001 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0264370716300333 http://hdl.handle.net/11336/46796 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Intraplate Compression Karoo Large Igneous Province Jurassic to Lower Cretaceous Inversion Supercontinent Break-Up https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.jog.2016.10.001 2024-10-04T09:34:05Z 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 Ca ?nadón Asfalto basins, during the earliest stages of breakup. A comparison with surrounding areas in Patagonia, where similar Juras-sic 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 expan-sion 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 (1) compatible with other Jurassic intraplate belts of South America. These observations led us to pro-pose 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. Fil: Navarrete Granzotto, César Rodrigo. Universidad Nacional de la Patagonia "San Juan Bosco"; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Gianni, Guido Martin. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Echaurren Gonzalez, Andres. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación ... Article in Journal/Newspaper Weddell Sea CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Weddell Sea Patagonia San Juan Weddell Argentina Chubut ENVELOPE(-62.533,-62.533,-76.100,-76.100) Sion ENVELOPE(13.758,13.758,66.844,66.844) Gonzalez ENVELOPE(-58.250,-58.250,-63.917,-63.917) Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Guido ENVELOPE(-60.933,-60.933,-64.050,-64.050) Navarrete ENVELOPE(-62.533,-62.533,-64.833,-64.833) Journal of Geodynamics 102 185 201
spellingShingle Intraplate Compression
Karoo Large Igneous Province
Jurassic to Lower Cretaceous Inversion
Supercontinent Break-Up
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Navarrete Granzotto, César Rodrigo
Gianni, Guido Martin
Echaurren Gonzalez, Andres
Lince Klinger, Federico Gustavo
Folguera Telichevsky, Andres
Episodic Jurassic to Lower Cretaceous intraplate compression in Central Patagonia during Gondwana breakup
title 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_short 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
topic Intraplate Compression
Karoo Large Igneous Province
Jurassic to Lower Cretaceous Inversion
Supercontinent Break-Up
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Intraplate Compression
Karoo Large Igneous Province
Jurassic to Lower Cretaceous Inversion
Supercontinent Break-Up
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/46796