Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics
We report the field geology, petrography, geochemistry and geochronology data for two dyke swarms in the Fuegian Andes, with the aim of correlating them with known suites and of improving the knowledge on the magmatism of the Late Cretaceous rear-arc and its relation with ductile deformation. We als...
Published in: | Journal of the Geological Society |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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Geological Society Publications House
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Online Access: | http://hdl.handle.net/11336/232658 |
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author | Gonzalez Guillot, Mauricio Alberto Torres Carbonell, Pablo Juan Cao, Sebastián José Lobo, Constanza Bordese, Sofía Hollanda, María Helena B.M. |
author_facet | Gonzalez Guillot, Mauricio Alberto Torres Carbonell, Pablo Juan Cao, Sebastián José Lobo, Constanza Bordese, Sofía Hollanda, María Helena B.M. |
author_sort | Gonzalez Guillot, Mauricio Alberto |
collection | CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) |
container_issue | 3 |
container_title | Journal of the Geological Society |
container_volume | 181 |
description | We report the field geology, petrography, geochemistry and geochronology data for two dyke swarms in the Fuegian Andes, with the aim of correlating them with known suites and of improving the knowledge on the magmatism of the Late Cretaceous rear-arc and its relation with ductile deformation. We also provide keys for correlation based on amphibole K2O content. The Trapecio dyke swarm is mildly alkaline and ferriferous, with a zircon U-Pb age of 75 Ma; thus it belongs to the Fuegian Potassic Magmatism (78-68 Ma). The Ushuaia Peninsula dyke swarm, also known as Ushuaia Peninsula Andesites (UPA), was shown to be high-K calc-alkaline and magnesian. New radiometric ages gave 87-86 Ma. While the UPA dyke swarm exhibits foliation associated with ductile deformation, the Trapecio dyke swarm is post-kinematic and reveals emplacement controlled by the slaty cleavage in the metapelite host. Field and geophysical evidence suggest both swarms overlie small upper-crustal plutons, mostly buried. The variable composition of dykes suggests a protracted history of dyke injection, mostly fed from deeper reservoirs. Contact metamorphism around both pluton-dyke systems is very weak. By comparison with adjacent plutons we argue that the main variables controlling aureole development are small magma volumes and low injection rates. Fil: Gonzalez Guillot, Mauricio Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina Fil: Torres Carbonell, Pablo Juan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Cao, Sebastián José. Universidad Nacional de Tierra del Fuego. Instituto de Ciencias Polares, Recursos Naturales y Ambiente; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias ... |
format | Article in Journal/Newspaper |
genre | Antártida Tierra del Fuego |
genre_facet | Antártida Tierra del Fuego |
geographic | Austral Argentina Gonzalez Pablo Ushuaia Carbonell Trapecio |
geographic_facet | Austral Argentina Gonzalez Pablo Ushuaia Carbonell Trapecio |
id | ftconicet:oai:ri.conicet.gov.ar:11336/232658 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-58.250,-58.250,-63.917,-63.917) ENVELOPE(-63.717,-63.717,-64.283,-64.283) ENVELOPE(-40.000,-40.000,-82.167,-82.167) ENVELOPE(-56.983,-56.983,-63.533,-63.533) ENVELOPE(-61.250,-61.250,-62.767,-62.767) |
op_collection_id | ftconicet |
op_doi | https://doi.org/10.1144/jgs2023-094 |
op_relation | info:eu-repo/semantics/altIdentifier/url/https://www.lyellcollection.org/doi/abs/10.1144/jgs2023-094 info:eu-repo/semantics/altIdentifier/doi/10.1144/jgs2023-094 http://hdl.handle.net/11336/232658 CONICET Digital CONICET |
op_rights | info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
publisher | Geological Society Publications House |
record_format | openpolar |
spelling | ftconicet:oai:ri.conicet.gov.ar:11336/232658 2025-01-16T19:46:45+00:00 Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics Gonzalez Guillot, Mauricio Alberto Torres Carbonell, Pablo Juan Cao, Sebastián José Lobo, Constanza Bordese, Sofía Hollanda, María Helena B.M. application/pdf http://hdl.handle.net/11336/232658 eng eng Geological Society Publications House info:eu-repo/semantics/altIdentifier/url/https://www.lyellcollection.org/doi/abs/10.1144/jgs2023-094 info:eu-repo/semantics/altIdentifier/doi/10.1144/jgs2023-094 http://hdl.handle.net/11336/232658 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Fuegian Andes Ushuaia 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/10.1144/jgs2023-094 2024-10-04T09:34:24Z We report the field geology, petrography, geochemistry and geochronology data for two dyke swarms in the Fuegian Andes, with the aim of correlating them with known suites and of improving the knowledge on the magmatism of the Late Cretaceous rear-arc and its relation with ductile deformation. We also provide keys for correlation based on amphibole K2O content. The Trapecio dyke swarm is mildly alkaline and ferriferous, with a zircon U-Pb age of 75 Ma; thus it belongs to the Fuegian Potassic Magmatism (78-68 Ma). The Ushuaia Peninsula dyke swarm, also known as Ushuaia Peninsula Andesites (UPA), was shown to be high-K calc-alkaline and magnesian. New radiometric ages gave 87-86 Ma. While the UPA dyke swarm exhibits foliation associated with ductile deformation, the Trapecio dyke swarm is post-kinematic and reveals emplacement controlled by the slaty cleavage in the metapelite host. Field and geophysical evidence suggest both swarms overlie small upper-crustal plutons, mostly buried. The variable composition of dykes suggests a protracted history of dyke injection, mostly fed from deeper reservoirs. Contact metamorphism around both pluton-dyke systems is very weak. By comparison with adjacent plutons we argue that the main variables controlling aureole development are small magma volumes and low injection rates. Fil: Gonzalez Guillot, Mauricio Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina Fil: Torres Carbonell, Pablo Juan. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Cao, Sebastián José. Universidad Nacional de Tierra del Fuego. Instituto de Ciencias Polares, Recursos Naturales y Ambiente; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias ... Article in Journal/Newspaper Antártida Tierra del Fuego CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Austral Argentina Gonzalez ENVELOPE(-58.250,-58.250,-63.917,-63.917) Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Ushuaia ENVELOPE(-40.000,-40.000,-82.167,-82.167) Carbonell ENVELOPE(-56.983,-56.983,-63.533,-63.533) Trapecio ENVELOPE(-61.250,-61.250,-62.767,-62.767) Journal of the Geological Society 181 3 |
spellingShingle | Fuegian Andes Ushuaia https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Gonzalez Guillot, Mauricio Alberto Torres Carbonell, Pablo Juan Cao, Sebastián José Lobo, Constanza Bordese, Sofía Hollanda, María Helena B.M. Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics |
title | Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics |
title_full | Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics |
title_fullStr | Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics |
title_full_unstemmed | Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics |
title_short | Field geology, petrology and geochronology of pluton-dyke systems, the Trapecio and Ushuaia Peninsula dyke swarms (Fuegian Andes): Emplacement conditions and relation with tectonics |
title_sort | field geology, petrology and geochronology of pluton-dyke systems, the trapecio and ushuaia peninsula dyke swarms (fuegian andes): emplacement conditions and relation with tectonics |
topic | Fuegian Andes Ushuaia https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
topic_facet | Fuegian Andes Ushuaia https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
url | http://hdl.handle.net/11336/232658 |