The gabbro-peridotite complex of Bosque Alegre, Cordoba Province

The gabbro-peridotite complex of Bosque Alegre crops out in a NNW-SSE trending belt 2 km long and 0.8 km wide, located 20 km SE of Villa Carlos Paz, Cordoba, Argentina. It was emplaced concordantly with rocks of the Precambrian crystalline basement which are dominantly of amphibolite facies. The ult...

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Autor principal: Mutti, D.I.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_NIS00264_v47_n2_p153_Mutti
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spelling todo:paper_NIS00264_v47_n2_p153_Mutti2023-10-03T16:45:37Z The gabbro-peridotite complex of Bosque Alegre, Cordoba Province Mutti, D.I. folding gabbro metamorphism peridotite serpentinization tectonics Argentina Bosque Alegre Cordoba The gabbro-peridotite complex of Bosque Alegre crops out in a NNW-SSE trending belt 2 km long and 0.8 km wide, located 20 km SE of Villa Carlos Paz, Cordoba, Argentina. It was emplaced concordantly with rocks of the Precambrian crystalline basement which are dominantly of amphibolite facies. The ultramafic-mafic rocks formed a folded differentiated igneous complex with peridotites at the base followed by pyroxenites, hornblendites and gabbros at the top. They are intensely serpentinized and uralitized and probably represent part of the roof zone of an old island arc and/or back arc system. Folding was syntectonic with the regional metamorphism and occurred during four tectonic phases accompanied by intense serpentinization of the ultramafic rocks and amphibolitization of the gabbroic rocks. -English summary Fil:Mutti, D.I. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_NIS00264_v47_n2_p153_Mutti
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic folding
gabbro
metamorphism
peridotite
serpentinization
tectonics
Argentina
Bosque Alegre
Cordoba
spellingShingle folding
gabbro
metamorphism
peridotite
serpentinization
tectonics
Argentina
Bosque Alegre
Cordoba
Mutti, D.I.
The gabbro-peridotite complex of Bosque Alegre, Cordoba Province
topic_facet folding
gabbro
metamorphism
peridotite
serpentinization
tectonics
Argentina
Bosque Alegre
Cordoba
description The gabbro-peridotite complex of Bosque Alegre crops out in a NNW-SSE trending belt 2 km long and 0.8 km wide, located 20 km SE of Villa Carlos Paz, Cordoba, Argentina. It was emplaced concordantly with rocks of the Precambrian crystalline basement which are dominantly of amphibolite facies. The ultramafic-mafic rocks formed a folded differentiated igneous complex with peridotites at the base followed by pyroxenites, hornblendites and gabbros at the top. They are intensely serpentinized and uralitized and probably represent part of the roof zone of an old island arc and/or back arc system. Folding was syntectonic with the regional metamorphism and occurred during four tectonic phases accompanied by intense serpentinization of the ultramafic rocks and amphibolitization of the gabbroic rocks. -English summary
format JOUR
author Mutti, D.I.
author_facet Mutti, D.I.
author_sort Mutti, D.I.
title The gabbro-peridotite complex of Bosque Alegre, Cordoba Province
title_short The gabbro-peridotite complex of Bosque Alegre, Cordoba Province
title_full The gabbro-peridotite complex of Bosque Alegre, Cordoba Province
title_fullStr The gabbro-peridotite complex of Bosque Alegre, Cordoba Province
title_full_unstemmed The gabbro-peridotite complex of Bosque Alegre, Cordoba Province
title_sort gabbro-peridotite complex of bosque alegre, cordoba province
url http://hdl.handle.net/20.500.12110/paper_NIS00264_v47_n2_p153_Mutti
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