Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges

Many of the veins enclosed within the Paleozoic basement of the Catalonian Coastal Ranges show severa1 common characteristics: low temperature of formation (between 75 and 200C), the presence of complex polisaline fluids and a certain relationship to the pretriassic paleosurface. Mineralogical compo...

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Detalles Bibliográficos
Autores: Cardellach López, Esteve, Canals i Sabaté, Àngels, Tritlla i Cambra, Jordi
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:1990
País:España
Institución:Universidad de Barcelona
Repositorio:Dipòsit Digital de la UB
OAI Identifier:oai:diposit.ub.edu:2445/18175
Acceso en línea:https://hdl.handle.net/2445/18175
Access Level:acceso abierto
Palabra clave:Serralada Litoral Catalana
Mineralogia
Catalan Coastal Range (Catalonia)
Mineralogy
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spelling Late and post-Hercyniam low temperature veins in the Catalonian Coastal RangesCardellach López, EsteveCanals i Sabaté, ÀngelsTritlla i Cambra, JordiSerralada Litoral CatalanaMineralogiaCatalan Coastal Range (Catalonia)MineralogyMany of the veins enclosed within the Paleozoic basement of the Catalonian Coastal Ranges show severa1 common characteristics: low temperature of formation (between 75 and 200C), the presence of complex polisaline fluids and a certain relationship to the pretriassic paleosurface. Mineralogical composition and age are variable, ranging from Pb-Zn veins with carbonate gangue of late Hercynian age through metal poor fluorite rich veins to barite rich veins of Triasssic age. Mineralizing fluids are not related to late Hercynianmagmatism and deposition took place in active fractures developed either in extensional as in compressive regimes.Universitat de Barcelona (UB). Institut de Cincias de la Terra Jaume Almera (ICTJA)1990info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://hdl.handle.net/2445/18175Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésReproducció del document publicat a http://www.raco.cat/index.php/ActaGeologica/article/view/75369Acta Geologica Hispanica, 1990, vol. 25, núm. 1-2, p. 75-81(c) Cardellach, et al., 1990info:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/181752026-05-27T06:46:51Z
dc.title.none.fl_str_mv Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
title Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
spellingShingle Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
Cardellach López, Esteve
Serralada Litoral Catalana
Mineralogia
Catalan Coastal Range (Catalonia)
Mineralogy
title_short Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
title_full Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
title_fullStr Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
title_full_unstemmed Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
title_sort Late and post-Hercyniam low temperature veins in the Catalonian Coastal Ranges
dc.creator.none.fl_str_mv Cardellach López, Esteve
Canals i Sabaté, Àngels
Tritlla i Cambra, Jordi
author Cardellach López, Esteve
author_facet Cardellach López, Esteve
Canals i Sabaté, Àngels
Tritlla i Cambra, Jordi
author_role author
author2 Canals i Sabaté, Àngels
Tritlla i Cambra, Jordi
author2_role author
author
dc.subject.none.fl_str_mv Serralada Litoral Catalana
Mineralogia
Catalan Coastal Range (Catalonia)
Mineralogy
topic Serralada Litoral Catalana
Mineralogia
Catalan Coastal Range (Catalonia)
Mineralogy
description Many of the veins enclosed within the Paleozoic basement of the Catalonian Coastal Ranges show severa1 common characteristics: low temperature of formation (between 75 and 200C), the presence of complex polisaline fluids and a certain relationship to the pretriassic paleosurface. Mineralogical composition and age are variable, ranging from Pb-Zn veins with carbonate gangue of late Hercynian age through metal poor fluorite rich veins to barite rich veins of Triasssic age. Mineralizing fluids are not related to late Hercynianmagmatism and deposition took place in active fractures developed either in extensional as in compressive regimes.
publishDate 1990
dc.date.none.fl_str_mv 1990
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/18175
url https://hdl.handle.net/2445/18175
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Reproducció del document publicat a http://www.raco.cat/index.php/ActaGeologica/article/view/75369
Acta Geologica Hispanica, 1990, vol. 25, núm. 1-2, p. 75-81
dc.rights.none.fl_str_mv (c) Cardellach, et al., 1990
info:eu-repo/semantics/openAccess
rights_invalid_str_mv (c) Cardellach, et al., 1990
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universitat de Barcelona (UB). Institut de Cincias de la Terra Jaume Almera (ICTJA)
publisher.none.fl_str_mv Universitat de Barcelona (UB). Institut de Cincias de la Terra Jaume Almera (ICTJA)
dc.source.none.fl_str_mv Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)
reponame:Dipòsit Digital de la UB
instname:Universidad de Barcelona
instname_str Universidad de Barcelona
reponame_str Dipòsit Digital de la UB
collection Dipòsit Digital de la UB
repository.name.fl_str_mv
repository.mail.fl_str_mv
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