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dc.contributor.author
Rapela, Carlos Washington  
dc.contributor.author
Hervé, Francisco  
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Pankhurst, Robert  
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Calderón, Mauricio  
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Fanning, Christopher Mark  
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Quezada, Paulo  
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Foix, Nicolas  
dc.date.available
2024-02-29T10:29:57Z  
dc.date.issued
2022  
dc.identifier.citation
The Chaitenia accretionary orogen of northwest Patagonia: new U-Pb SHRIMP ages of the Foreland Domain; XXI Congreso Geológico Argentino; Puerto Madryn; Argentina; 2022; 1511-1512  
dc.identifier.isbn
978-987-48319-9-6  
dc.identifier.uri
http://hdl.handle.net/11336/228872  
dc.description.abstract
The Andean basement of NW Patagonia between 39º and 43º S contains remnants of Devonian plutonic, volcanic and metamorphic rocks. While some of them were clearly emplaced in continental crust at the easternmost edge of North Patagonian Massif, in the west of the North Patagonian Cordillera and the coastal region, the igneous rocks were developed in an oceanic environment. Thus, a Foreland Devonian Domain (FDD) and a Pacifi c Devonian Domain (PDD) are distinguished on either side of the modern Andean Cordillera (Fig. 1). While the Devonian granites of the Foreland Domain can be unambiguously ascribed to subduction in a continental margin (see references in Rapela et al. 2021), the more scattered outcrops of pillow lavas, alkaline trachyte-rhyolite and primitive granites of the PDD required more detailed studies to determine their petrogenesis and tectonic signifi cance. Initial studies suggested that they represented the mixed products of an oceanic island arc that later became accreted to the continent as an allochthonous terrane (the Chaitenia terrane of Hervé et al. 2016). However, whole-rock geochemistry shows that the pillow lavas are dominated by back-arc basalts and that metasandstones interbedded with the pillow lavas contain detrital zircons with U-Pb ages, Hf and O isotope compositions comparable to those of the Foreland Domain granites, i.e., they are of contemporary continental provenance. Thus, they are more likely to represent a Devonian parautochthonous terrane, formed after continental rifting and was laterally accreted during closure of a back-arc basin in an orogen that also encompasses the fore-arc (Rapela et al. 2021), and which we now refer to as the Chaitenia Accretionary Orogen (CAO). Five stages have been recognized in its evolution: (i) a continental arc stage that involved the San Martín arc (c. 405-395 Ma, Emsian); (ii) a forearc rift-ridge transition stage (c. 395-390 Ma, Emsian-Eifelian); (iii) a marginal basin stage that involves the starting of an oceanic arc, the Chaitenia arc (c. 380-390 Ma, Eifelian-Givetian); (iv) a double arc stage (365-380 Ma, Giovetian-Frasnian) and (v) closing of the Chaitenia marginal basin (c. 360-340 Ma, Fammenian-Visean).  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Asociación Geológica Argentina  
dc.rights
info:eu-repo/semantics/openAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
Patagonian Cordillera  
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Devonian magmatism  
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Geochronology  
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Geochemistry  
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Geoquímica y Geofísica  
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Ciencias de la Tierra y relacionadas con el Medio Ambiente  
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CIENCIAS NATURALES Y EXACTAS  
dc.title
The Chaitenia accretionary orogen of northwest Patagonia: new U-Pb SHRIMP ages of the Foreland Domain  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.type
info:eu-repo/semantics/conferenceObject  
dc.type
info:ar-repo/semantics/documento de conferencia  
dc.date.updated
2024-02-22T14:20:49Z  
dc.journal.pagination
1511-1512  
dc.journal.pais
Argentina  
dc.journal.ciudad
Ciudad Autónoma de Buenos Aires  
dc.description.fil
Fil: Rapela, Carlos Washington. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina  
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Fil: Hervé, Francisco. Universidad Andrés Bello; Chile  
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Fil: Pankhurst, Robert. British Geological Survey; Reino Unido  
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Fil: Calderón, Mauricio. Universidad Andrés Bello; Chile  
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Fil: Fanning, Christopher Mark. Australian National University; Australia  
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Fil: Quezada, Paulo. Universidade Tecnologia Federal Do Parana.; Brasil  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://geologica.org.ar/xxi-cga-2022-chubut/  
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Autor  
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Autor  
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Autor  
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Autor  
dc.conicet.rol
Autor  
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Autor  
dc.coverage
Nacional  
dc.type.subtype
Congreso  
dc.description.nombreEvento
XXI Congreso Geológico Argentino  
dc.date.evento
2022-03-14  
dc.description.ciudadEvento
Puerto Madryn  
dc.description.paisEvento
Argentina  
dc.type.publicacion
Book  
dc.description.institucionOrganizadora
Asociación Geológica Argentina  
dc.source.libro
Actas del XXI Congreso Geológico Argentino  
dc.date.eventoHasta
2022-03-18  
dc.type
Congreso