The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution
- Autores
- Guido, Diego Martin; Escayola, Monica Patricia; Schalamuk, Bernardo Isidoro
- Año de publicación
- 2004
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Rı́o Deseado Complex, the basement of the eastern Deseado Massif geological province of Argentina, is composed of five dispersed, small outcrops of upper Proterozoic–lower Paleozoic metamorphic and igneous rocks. We propose a possible evolution for these rocks on the basis of a detailed study of the easternmost outcrop (Bahı́a Laura). The Bahı́a Laura metamorphic rocks are metasedimentary and igneous-derived rocks formed prior to the Pampean metamorphic event. Metasedimentary schists, garnet-rich and micaceous gneisses, and the migmatite's paleosome are interpreted as marine sediments (pelites, sandstones, and limestones). The igneous-derived rocks are metaluminous and peraluminous granodiorites (hornblendic and granodioritic gneisses) and tholeiitic basalts (amphibolites) that were produced in a magmatic arc and a primitive island arc, respectively. These rocks underwent regional metamorphism during the Pampean cycle (Neoproterozoic–Paleozoic boundary), then a plutonic intrusion (Bahı́a Laura peraluminous monzogranite) and several granitoid injections,both of which are correlated with the Famatinian (Ordovician–Silurian) magmatic arc proposed for this region. Finally, all rocks were slightly deformed by a post-Famatinian tectonic event that may have produced the basement exhumation. According to the proposed evolution of the Rı́o Deseado Complex in Bahı́a Laura, the basement of the Deseado Massif could be part of a Late Proterozoic-Mid Paleozoic orogenic belt.
Fil: Guido, Diego Martin. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Recursos Minerales. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas. Instituto de Recursos Minerales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Escayola, Monica Patricia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina
Fil: Schalamuk, Bernardo Isidoro. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Recursos Minerales. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas. Instituto de Recursos Minerales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina - Materia
-
BAHÍA LAURA
BASEMENT
DESEADO MASSIF
RO DESEADO COMPLEX - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/95105
Ver los metadatos del registro completo
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The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolutionGuido, Diego MartinEscayola, Monica PatriciaSchalamuk, Bernardo IsidoroBAHÍA LAURABASEMENTDESEADO MASSIFRO DESEADO COMPLEXhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Rı́o Deseado Complex, the basement of the eastern Deseado Massif geological province of Argentina, is composed of five dispersed, small outcrops of upper Proterozoic–lower Paleozoic metamorphic and igneous rocks. We propose a possible evolution for these rocks on the basis of a detailed study of the easternmost outcrop (Bahı́a Laura). The Bahı́a Laura metamorphic rocks are metasedimentary and igneous-derived rocks formed prior to the Pampean metamorphic event. Metasedimentary schists, garnet-rich and micaceous gneisses, and the migmatite's paleosome are interpreted as marine sediments (pelites, sandstones, and limestones). The igneous-derived rocks are metaluminous and peraluminous granodiorites (hornblendic and granodioritic gneisses) and tholeiitic basalts (amphibolites) that were produced in a magmatic arc and a primitive island arc, respectively. These rocks underwent regional metamorphism during the Pampean cycle (Neoproterozoic–Paleozoic boundary), then a plutonic intrusion (Bahı́a Laura peraluminous monzogranite) and several granitoid injections,both of which are correlated with the Famatinian (Ordovician–Silurian) magmatic arc proposed for this region. Finally, all rocks were slightly deformed by a post-Famatinian tectonic event that may have produced the basement exhumation. According to the proposed evolution of the Rı́o Deseado Complex in Bahı́a Laura, the basement of the Deseado Massif could be part of a Late Proterozoic-Mid Paleozoic orogenic belt.Fil: Guido, Diego Martin. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Recursos Minerales. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas. Instituto de Recursos Minerales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Escayola, Monica Patricia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; ArgentinaFil: Schalamuk, Bernardo Isidoro. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Recursos Minerales. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas. Instituto de Recursos Minerales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaPergamon-Elsevier Science Ltd2004-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/95105Guido, Diego Martin; Escayola, Monica Patricia; Schalamuk, Bernardo Isidoro; The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 7; 4-2004; 567-5770895-9811CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981103001524info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2003.10.003info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T15:09:18Zoai:ri.conicet.gov.ar:11336/95105instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-15 15:09:18.57CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution |
title |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution |
spellingShingle |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution Guido, Diego Martin BAHÍA LAURA BASEMENT DESEADO MASSIF RO DESEADO COMPLEX |
title_short |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution |
title_full |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution |
title_fullStr |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution |
title_full_unstemmed |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution |
title_sort |
The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution |
dc.creator.none.fl_str_mv |
Guido, Diego Martin Escayola, Monica Patricia Schalamuk, Bernardo Isidoro |
author |
Guido, Diego Martin |
author_facet |
Guido, Diego Martin Escayola, Monica Patricia Schalamuk, Bernardo Isidoro |
author_role |
author |
author2 |
Escayola, Monica Patricia Schalamuk, Bernardo Isidoro |
author2_role |
author author |
dc.subject.none.fl_str_mv |
BAHÍA LAURA BASEMENT DESEADO MASSIF RO DESEADO COMPLEX |
topic |
BAHÍA LAURA BASEMENT DESEADO MASSIF RO DESEADO COMPLEX |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Rı́o Deseado Complex, the basement of the eastern Deseado Massif geological province of Argentina, is composed of five dispersed, small outcrops of upper Proterozoic–lower Paleozoic metamorphic and igneous rocks. We propose a possible evolution for these rocks on the basis of a detailed study of the easternmost outcrop (Bahı́a Laura). The Bahı́a Laura metamorphic rocks are metasedimentary and igneous-derived rocks formed prior to the Pampean metamorphic event. Metasedimentary schists, garnet-rich and micaceous gneisses, and the migmatite's paleosome are interpreted as marine sediments (pelites, sandstones, and limestones). The igneous-derived rocks are metaluminous and peraluminous granodiorites (hornblendic and granodioritic gneisses) and tholeiitic basalts (amphibolites) that were produced in a magmatic arc and a primitive island arc, respectively. These rocks underwent regional metamorphism during the Pampean cycle (Neoproterozoic–Paleozoic boundary), then a plutonic intrusion (Bahı́a Laura peraluminous monzogranite) and several granitoid injections,both of which are correlated with the Famatinian (Ordovician–Silurian) magmatic arc proposed for this region. Finally, all rocks were slightly deformed by a post-Famatinian tectonic event that may have produced the basement exhumation. According to the proposed evolution of the Rı́o Deseado Complex in Bahı́a Laura, the basement of the Deseado Massif could be part of a Late Proterozoic-Mid Paleozoic orogenic belt. Fil: Guido, Diego Martin. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Recursos Minerales. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas. Instituto de Recursos Minerales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Escayola, Monica Patricia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Salta. Facultad de Ciencias Naturales. Instituto Geonorte; Argentina Fil: Schalamuk, Bernardo Isidoro. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Instituto de Recursos Minerales. Provincia de Buenos Aires. Gobernación. Comisión de Investigaciones Científicas. Instituto de Recursos Minerales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina |
description |
The Rı́o Deseado Complex, the basement of the eastern Deseado Massif geological province of Argentina, is composed of five dispersed, small outcrops of upper Proterozoic–lower Paleozoic metamorphic and igneous rocks. We propose a possible evolution for these rocks on the basis of a detailed study of the easternmost outcrop (Bahı́a Laura). The Bahı́a Laura metamorphic rocks are metasedimentary and igneous-derived rocks formed prior to the Pampean metamorphic event. Metasedimentary schists, garnet-rich and micaceous gneisses, and the migmatite's paleosome are interpreted as marine sediments (pelites, sandstones, and limestones). The igneous-derived rocks are metaluminous and peraluminous granodiorites (hornblendic and granodioritic gneisses) and tholeiitic basalts (amphibolites) that were produced in a magmatic arc and a primitive island arc, respectively. These rocks underwent regional metamorphism during the Pampean cycle (Neoproterozoic–Paleozoic boundary), then a plutonic intrusion (Bahı́a Laura peraluminous monzogranite) and several granitoid injections,both of which are correlated with the Famatinian (Ordovician–Silurian) magmatic arc proposed for this region. Finally, all rocks were slightly deformed by a post-Famatinian tectonic event that may have produced the basement exhumation. According to the proposed evolution of the Rı́o Deseado Complex in Bahı́a Laura, the basement of the Deseado Massif could be part of a Late Proterozoic-Mid Paleozoic orogenic belt. |
publishDate |
2004 |
dc.date.none.fl_str_mv |
2004-04 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/95105 Guido, Diego Martin; Escayola, Monica Patricia; Schalamuk, Bernardo Isidoro; The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 7; 4-2004; 567-577 0895-9811 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/95105 |
identifier_str_mv |
Guido, Diego Martin; Escayola, Monica Patricia; Schalamuk, Bernardo Isidoro; The basement of the Deseado Massif at Bahı́a Laura, Patagonia, Argentina: a proposal for its evolution; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 16; 7; 4-2004; 567-577 0895-9811 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981103001524 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2003.10.003 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Pergamon-Elsevier Science Ltd |
publisher.none.fl_str_mv |
Pergamon-Elsevier Science Ltd |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1846083240557805568 |
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13.22299 |