Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques

Bertrab Nunatak is located in the Vahsel Bay area, Weddell Sea, Antarctica. It is composed of a granitic body, «Granito Bertrab», cut by acid­ aplite/rhyolite and quartz veins) and basic dyke-swarms. Granito Bertrab is a coarse-grained, granophyric quartz-feldspar biotite granite with minor normativ...

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Main Authors: Acevedo, Rogelio Daniel, Linares, Enrique, Alberdi Valin, Maria Luz, Ostera, Hector Adolfo, Martín Izard, Agustín
Format: Article in Journal/Newspaper
Language:Spanish
Published: Asociación Geológica Argentina
Subjects:
Online Access:http://hdl.handle.net/11336/156199
id ftconicet:oai:ri.conicet.gov.ar:11336/156199
record_format openpolar
spelling ftconicet:oai:ri.conicet.gov.ar:11336/156199 2023-10-09T21:45:32+02:00 Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques Acevedo, Rogelio Daniel Linares, Enrique Alberdi Valin, Maria Luz Ostera, Hector Adolfo Martín Izard, Agustín application/pdf http://hdl.handle.net/11336/156199 spa spa Asociación Geológica Argentina info:eu-repo/semantics/altIdentifier/url/https://revista.geologica.org.ar/raga/issue/view/23 http://hdl.handle.net/11336/156199 Acevedo, Rogelio Daniel; Linares, Enrique; Alberdi Valin, Maria Luz; Ostera, Hector Adolfo; Martín Izard, Agustín; Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques; Asociación Geológica Argentina; Revista de la Asociación Geológica Argentina; 55; 3; 12-2000; 179-187 0004-4822 1851-8249 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc/2.5/ar/ GRANITO BERTRAB EDAD ISOTÓPICA ANTÁRTIDA 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 2023-09-24T18:51:49Z Bertrab Nunatak is located in the Vahsel Bay area, Weddell Sea, Antarctica. It is composed of a granitic body, «Granito Bertrab», cut by acid­ aplite/rhyolite and quartz veins) and basic dyke-swarms. Granito Bertrab is a coarse-grained, granophyric quartz-feldspar biotite granite with minor normative corundum (1%) that indicates peraluminous affinities. Melanocratic calc-alkaline dykes, with labradorite-andesine and amphibole megacrysts, have a lamprophyric character. One of these is cut by a leucocratic dike, that represents the final stage in the magmatic activity. Petrological evidence indicates that there is a temporally, spatially and genetically intimate association bewteen the granite and the dykes. K-Ar data on samples of the granite give an age of 996 ± 40 Ma, and the Rb-Sr isochron age recalculated using the published data of Eastin and Faure give an age of 971 ± 8 Ma using five samples, and 992 ± 12 Ma when the aplitic member is not included. These results are in good agreement with the K-Ar age and mean that the Granito Bertrab was emplaced in the late Mesoproterozoic. Fil: Acevedo, Rogelio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Linares, Enrique. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotópica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; Argentina Fil: Alberdi Valin, Maria Luz. Universidad de Oviedo; España Fil: Ostera, Hector Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotópica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; Argentina Fil: Martín Izard, Agustín. Universidad de Oviedo; España Article in Journal/Newspaper Antarc* Antarctica Antártida Vahsel Bay Weddell Sea CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Austral Bertrab ENVELOPE(-34.533,-34.533,-77.917,-77.917) Bertrab nunatak ENVELOPE(-34.633,-34.633,-77.883,-77.883) Faure ENVELOPE(-68.871,-68.871,-68.093,-68.093) Granito ENVELOPE(-60.783,-60.783,-62.450,-62.450) Hector ENVELOPE(-63.376,-63.376,-64.579,-64.579) Vahsel ENVELOPE(-35.117,-35.117,-77.817,-77.817) Vahsel Bay ENVELOPE(-35.166,-35.166,-77.816,-77.816) Weddell Weddell Sea
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language Spanish
topic GRANITO BERTRAB
EDAD ISOTÓPICA
ANTÁRTIDA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
spellingShingle GRANITO BERTRAB
EDAD ISOTÓPICA
ANTÁRTIDA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Acevedo, Rogelio Daniel
Linares, Enrique
Alberdi Valin, Maria Luz
Ostera, Hector Adolfo
Martín Izard, Agustín
Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques
topic_facet GRANITO BERTRAB
EDAD ISOTÓPICA
ANTÁRTIDA
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description Bertrab Nunatak is located in the Vahsel Bay area, Weddell Sea, Antarctica. It is composed of a granitic body, «Granito Bertrab», cut by acid­ aplite/rhyolite and quartz veins) and basic dyke-swarms. Granito Bertrab is a coarse-grained, granophyric quartz-feldspar biotite granite with minor normative corundum (1%) that indicates peraluminous affinities. Melanocratic calc-alkaline dykes, with labradorite-andesine and amphibole megacrysts, have a lamprophyric character. One of these is cut by a leucocratic dike, that represents the final stage in the magmatic activity. Petrological evidence indicates that there is a temporally, spatially and genetically intimate association bewteen the granite and the dykes. K-Ar data on samples of the granite give an age of 996 ± 40 Ma, and the Rb-Sr isochron age recalculated using the published data of Eastin and Faure give an age of 971 ± 8 Ma using five samples, and 992 ± 12 Ma when the aplitic member is not included. These results are in good agreement with the K-Ar age and mean that the Granito Bertrab was emplaced in the late Mesoproterozoic. Fil: Acevedo, Rogelio Daniel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Linares, Enrique. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotópica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; Argentina Fil: Alberdi Valin, Maria Luz. Universidad de Oviedo; España Fil: Ostera, Hector Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geocronología y Geología Isotópica. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geocronología y Geología Isotópica; Argentina Fil: Martín Izard, Agustín. Universidad de Oviedo; España
format Article in Journal/Newspaper
author Acevedo, Rogelio Daniel
Linares, Enrique
Alberdi Valin, Maria Luz
Ostera, Hector Adolfo
Martín Izard, Agustín
author_facet Acevedo, Rogelio Daniel
Linares, Enrique
Alberdi Valin, Maria Luz
Ostera, Hector Adolfo
Martín Izard, Agustín
author_sort Acevedo, Rogelio Daniel
title Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques
title_short Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques
title_full Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques
title_fullStr Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques
title_full_unstemmed Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques
title_sort plutonismo proterozoico en antártida: el granito bertrab y su cortejo de diques
publisher Asociación Geológica Argentina
url http://hdl.handle.net/11336/156199
long_lat ENVELOPE(-34.533,-34.533,-77.917,-77.917)
ENVELOPE(-34.633,-34.633,-77.883,-77.883)
ENVELOPE(-68.871,-68.871,-68.093,-68.093)
ENVELOPE(-60.783,-60.783,-62.450,-62.450)
ENVELOPE(-63.376,-63.376,-64.579,-64.579)
ENVELOPE(-35.117,-35.117,-77.817,-77.817)
ENVELOPE(-35.166,-35.166,-77.816,-77.816)
geographic Argentina
Austral
Bertrab
Bertrab nunatak
Faure
Granito
Hector
Vahsel
Vahsel Bay
Weddell
Weddell Sea
geographic_facet Argentina
Austral
Bertrab
Bertrab nunatak
Faure
Granito
Hector
Vahsel
Vahsel Bay
Weddell
Weddell Sea
genre Antarc*
Antarctica
Antártida
Vahsel Bay
Weddell Sea
genre_facet Antarc*
Antarctica
Antártida
Vahsel Bay
Weddell Sea
op_relation info:eu-repo/semantics/altIdentifier/url/https://revista.geologica.org.ar/raga/issue/view/23
http://hdl.handle.net/11336/156199
Acevedo, Rogelio Daniel; Linares, Enrique; Alberdi Valin, Maria Luz; Ostera, Hector Adolfo; Martín Izard, Agustín; Plutonismo proterozoico en Antártida: el Granito Bertrab y su cortejo de diques; Asociación Geológica Argentina; Revista de la Asociación Geológica Argentina; 55; 3; 12-2000; 179-187
0004-4822
1851-8249
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc/2.5/ar/
_version_ 1779319616298811392