Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa?
The Pampean orogeny of northern Argentina resulted from Early Cambrian oblique collision of the Paleoproterozoic-Mesoproterozoic MARA block, formerly attached to Laurentia, with the Gondwanan Kalahari and Rio de la Plata cratons. The orogen is partially preserved because it is bounded by the younger...
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ftconicet:oai:ri.conicet.gov.ar:11336/45895 2023-10-09T21:45:37+02:00 Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa? Casquet, César Dahlquist, Juan Andrés Verdecchia, Sebastián Osvaldo Baldo, Edgardo Gaspar Agustín Galindo, Carmen Rapela, Carlos Washington Pankhurst, Robert J. Morales Camera, Matías Martín Murra, Juan Alberto Félix Fanning, Christopher Mark application/pdf http://hdl.handle.net/11336/45895 eng eng Elsevier Science info:eu-repo/semantics/altIdentifier/doi/10.1016/j.earscirev.2017.11.013 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0012825217302878 http://hdl.handle.net/11336/45895 Casquet, César; Dahlquist, Juan Andrés; Verdecchia, Sebastián Osvaldo; Baldo, Edgardo Gaspar Agustín; Galindo, Carmen; et al.; Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa?; Elsevier Science; Earth-science Reviews; 177; 2-2018; 209-225 0012-8252 CONICET Digital CONICET info:eu-repo/semantics/embargoedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ COLLISIONAL OROGENY GONDWANA MARA TERRANE PAMPEAN OROGENY SALDANIAN OROGENY SIERRAS PAMPEANAS 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.earscirev.2017.11.013 2023-09-24T19:06:55Z The Pampean orogeny of northern Argentina resulted from Early Cambrian oblique collision of the Paleoproterozoic-Mesoproterozoic MARA block, formerly attached to Laurentia, with the Gondwanan Kalahari and Rio de la Plata cratons. The orogen is partially preserved because it is bounded by the younger Córdoba Fault on the east and by the Los Túneles-Guacha Corral Ordovician shear zone on the west. In this review we correlate the Pampean Belt with the Saldania orogenic belt of South Africa and argue that both formed at an active continental margin fed with sediments coming mainly from the erosion of the Brasiliano–Pan-African and East African–Antarctica orogens between ca. 570 and 537 Ma (Puncoviscana Formation) and between 557 and 552 Ma (Malmesbury Group) respectively. Magmatic arcs (I-type and S-type granitoids) formed at the margin between ca. 552 and 530 Ma. Further right-lateral oblique collision of MARA between ca. 530 and 520 Ma produced a westward verging thickened belt. This involved an upper plate with high P/T metamorphism and a lower plate with high-grade intermediate to high P/T metamorphism probably resulting from crustal delamination or root foundering. The Neoproterozoic to Early Cambrian sedimentary cover of MARA that was part of the lower plate is only recognized in the high-grade domain along with a dismembered mafic–ultramafic ophiolite probably obducted in the early stages of collision. Uplift was fast in the upper plate and slower in the lower plate. Eventually the Saldania and Pampean belts detached from each other along the right-lateral Córdoba Fault, juxtaposing the Rio de la Plata craton against the internal high-grade zone of the Pampean belt. Fil: Casquet, César. Universidad Complutense de Madrid; España Fil: Dahlquist, Juan Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de ... Article in Journal/Newspaper Antarc* Antarctica CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Corral ENVELOPE(-62.950,-62.950,-64.900,-64.900) Mara ENVELOPE(132.133,132.133,62.267,62.267) Earth-Science Reviews 177 209 225 |
institution |
Open Polar |
collection |
CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
op_collection_id |
ftconicet |
language |
English |
topic |
COLLISIONAL OROGENY GONDWANA MARA TERRANE PAMPEAN OROGENY SALDANIAN OROGENY SIERRAS PAMPEANAS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
spellingShingle |
COLLISIONAL OROGENY GONDWANA MARA TERRANE PAMPEAN OROGENY SALDANIAN OROGENY SIERRAS PAMPEANAS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Casquet, César Dahlquist, Juan Andrés Verdecchia, Sebastián Osvaldo Baldo, Edgardo Gaspar Agustín Galindo, Carmen Rapela, Carlos Washington Pankhurst, Robert J. Morales Camera, Matías Martín Murra, Juan Alberto Félix Fanning, Christopher Mark Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa? |
topic_facet |
COLLISIONAL OROGENY GONDWANA MARA TERRANE PAMPEAN OROGENY SALDANIAN OROGENY SIERRAS PAMPEANAS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
description |
The Pampean orogeny of northern Argentina resulted from Early Cambrian oblique collision of the Paleoproterozoic-Mesoproterozoic MARA block, formerly attached to Laurentia, with the Gondwanan Kalahari and Rio de la Plata cratons. The orogen is partially preserved because it is bounded by the younger Córdoba Fault on the east and by the Los Túneles-Guacha Corral Ordovician shear zone on the west. In this review we correlate the Pampean Belt with the Saldania orogenic belt of South Africa and argue that both formed at an active continental margin fed with sediments coming mainly from the erosion of the Brasiliano–Pan-African and East African–Antarctica orogens between ca. 570 and 537 Ma (Puncoviscana Formation) and between 557 and 552 Ma (Malmesbury Group) respectively. Magmatic arcs (I-type and S-type granitoids) formed at the margin between ca. 552 and 530 Ma. Further right-lateral oblique collision of MARA between ca. 530 and 520 Ma produced a westward verging thickened belt. This involved an upper plate with high P/T metamorphism and a lower plate with high-grade intermediate to high P/T metamorphism probably resulting from crustal delamination or root foundering. The Neoproterozoic to Early Cambrian sedimentary cover of MARA that was part of the lower plate is only recognized in the high-grade domain along with a dismembered mafic–ultramafic ophiolite probably obducted in the early stages of collision. Uplift was fast in the upper plate and slower in the lower plate. Eventually the Saldania and Pampean belts detached from each other along the right-lateral Córdoba Fault, juxtaposing the Rio de la Plata craton against the internal high-grade zone of the Pampean belt. Fil: Casquet, César. Universidad Complutense de Madrid; España Fil: Dahlquist, Juan Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de ... |
format |
Article in Journal/Newspaper |
author |
Casquet, César Dahlquist, Juan Andrés Verdecchia, Sebastián Osvaldo Baldo, Edgardo Gaspar Agustín Galindo, Carmen Rapela, Carlos Washington Pankhurst, Robert J. Morales Camera, Matías Martín Murra, Juan Alberto Félix Fanning, Christopher Mark |
author_facet |
Casquet, César Dahlquist, Juan Andrés Verdecchia, Sebastián Osvaldo Baldo, Edgardo Gaspar Agustín Galindo, Carmen Rapela, Carlos Washington Pankhurst, Robert J. Morales Camera, Matías Martín Murra, Juan Alberto Félix Fanning, Christopher Mark |
author_sort |
Casquet, César |
title |
Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa? |
title_short |
Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa? |
title_full |
Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa? |
title_fullStr |
Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa? |
title_full_unstemmed |
Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa? |
title_sort |
review of the cambrian pampean orogeny of argentina; a displaced orogen formerly attached to the saldania belt of south africa? |
publisher |
Elsevier Science |
url |
http://hdl.handle.net/11336/45895 |
long_lat |
ENVELOPE(-62.950,-62.950,-64.900,-64.900) ENVELOPE(132.133,132.133,62.267,62.267) |
geographic |
Argentina Corral Mara |
geographic_facet |
Argentina Corral Mara |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.earscirev.2017.11.013 info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0012825217302878 http://hdl.handle.net/11336/45895 Casquet, César; Dahlquist, Juan Andrés; Verdecchia, Sebastián Osvaldo; Baldo, Edgardo Gaspar Agustín; Galindo, Carmen; et al.; Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa?; Elsevier Science; Earth-science Reviews; 177; 2-2018; 209-225 0012-8252 CONICET Digital CONICET |
op_rights |
info:eu-repo/semantics/embargoedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
op_doi |
https://doi.org/10.1016/j.earscirev.2017.11.013 |
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Earth-Science Reviews |
container_volume |
177 |
container_start_page |
209 |
op_container_end_page |
225 |
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1779320341649162240 |