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dc.contributor.author
Rapela, Carlos Washington
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dc.contributor.author
Hervé, Francisco
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dc.contributor.author
Pankhurst, Robert John
dc.contributor.author
Calderón, Mauricio
dc.contributor.author
Fanning, Christopher Mark
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dc.contributor.author
Quezada, Paulo
dc.contributor.author
Poblete, Fernando
dc.contributor.author
Palape, Camilo
dc.contributor.author
Reyes, Tomas
dc.date.available
2022-01-28T15:14:44Z
dc.date.issued
2021-08
dc.identifier.citation
Rapela, Carlos Washington; Hervé, Francisco; Pankhurst, Robert John; Calderón, Mauricio; Fanning, Christopher Mark; et al.; The Devonian accretionary orogen of the North Patagonian cordillera; Elsevier Science; Gondwana Research; 96; 8-2021; 1-21
dc.identifier.issn
1342-937X
dc.identifier.uri
http://hdl.handle.net/11336/150890
dc.description.abstract
The Andean basement of NW Patagonia contains remnants of a Devonian accretionary orogen that lasted for about 50 Ma. We present and review U-Pb geochronology, major and trace element geochemistry and O- and Hf-isotope analyses of zircon for Devonian igneous and metasedimentary rocks from the western edge of the North Patagonian Massif to the Pacific coast. Two contrasting magmatic domains are characterised. The Foreland Devonian Domain (FDD) of the North Patagonian Massif is dominated by subduction-related calcalkaline granite, granodiorite and tonalite emplaced in the interval c. 405–395 Ma and here named the San Martín arc. They are generally enriched in alkalis, light rare earth and Large Ion Lithophile elements, and have igneous zircon with δ18O mostly in the range +6 to +9‰ and ƐHft typically +3 to −5, indicating magmas that incorporated continental crustal material, possibly Mesoproterozoic. A younger (374 ± 3 Ma) body in this group has lower δ18O (down to +5‰) and Hf-isotope characteristics at the primitive end of this range. The Pacific Devonian Domain (PDD) lies on the western flank of the Andes and has uniformly primitive character. Granitic rocks here represent a more extended magmatic history (c. 395–355 Ma) and are mostly subalkaline tonalites with δ18O (<+6‰) that fall within or below the normal mantle field: with one exception their ɛHft values are > +4 and closer to Devonian depleted mantle composition. The PDD also has metabasalts of both N-MORB and E-MORB affinities, interbedded with Devonian turbidite metasandstones in which detrital zircon O- and Hf-isotope compositions and morphology indicate coetaneous derivation from the FDD arc. The results lead to a tectonic model involving continental arc, forearc rifting, Chaitenia oceanic arc and marginal basin formation, double arc subduction, and marginal basin closure in Mississippian times. This is recognisable as part of a more extensive Devonian accretion scenario along the SW Gondwana margin.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Elsevier Science
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dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
DEVONIAN OROGEN
dc.subject
MARGINAL BASIN
dc.subject
O-HF ISOTOPES
dc.subject
PATAGONIA
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ZIRCON DATING
dc.subject.classification
Geoquímica y Geofísica
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dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente
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dc.subject.classification
CIENCIAS NATURALES Y EXACTAS
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dc.title
The Devonian accretionary orogen of the North Patagonian cordillera
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2022-01-27T18:13:22Z
dc.journal.volume
96
dc.journal.pagination
1-21
dc.journal.pais
Países Bajos
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dc.journal.ciudad
Amsterdam
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
dc.description.fil
Fil: Hervé, Francisco. Universidad de Chile; Chile. Universidad Andrés Bello; Chile
dc.description.fil
Fil: Pankhurst, Robert John. British Geological Survey (bgs); Reino Unido
dc.description.fil
Fil: Calderón, Mauricio. Universidad Andrés Bello; Chile
dc.description.fil
Fil: Fanning, Christopher Mark. The Australian National University; Australia
dc.description.fil
Fil: Quezada, Paulo. Universidade Federal do Paraná; Brasil
dc.description.fil
Fil: Poblete, Fernando. Universidad de Chile; Chile
dc.description.fil
Fil: Palape, Camilo. Universidad Andrés Bello; Chile
dc.description.fil
Fil: Reyes, Tomas. Universidad Andrés Bello; Chile. Universidad de Chile; Chile
dc.journal.title
Gondwana Research
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dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.gr.2021.04.004
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1342937X21001258?via%3Dihub
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