The late Miocene Campo Coy gypsum (Eastern Betics, Spain)

The Campo Coy basin contains an important evaporite succession, up to 350 meters thick of gypsum, including two gypsum units: lower and upper gypsum units. These are characterized by fine-grain laminated and selenitic primary gypsums and by nodular-laminated and meganodular secondary gypsums. The ge...

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Detalles Bibliográficos
Autores: Artiaga Torres, David, García Veigas, Javier, Gibert Beotas, Luis, Soria, Jesús M.
Tipo de recurso: artículo
Fecha de publicación:2020
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:inglés
OAI Identifier:oai:ariasmontano.uhu.es:10272/18587
Acceso en línea:http://hdl.handle.net/10272/18587
Access Level:acceso abierto
Palabra clave:Evaporites
Geochemistry
Neogene Betic basins
Evaporitas
Geoquímica
Cuencas neógenas Béticas
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spelling The late Miocene Campo Coy gypsum (Eastern Betics, Spain)Los yesos del Mioceno superior de Campo Coy (Cordillera Bética oriental, España)Artiaga Torres, DavidGarcía Veigas, JavierGibert Beotas, LuisSoria, Jesús M.EvaporitesGeochemistryNeogene Betic basinsEvaporitasGeoquímicaCuencas neógenas BéticasThe Campo Coy basin contains an important evaporite succession, up to 350 meters thick of gypsum, including two gypsum units: lower and upper gypsum units. These are characterized by fine-grain laminated and selenitic primary gypsums and by nodular-laminated and meganodular secondary gypsums. The geochemical study based on sulfate isotope compositions (δ34S and δ18O) and strontium isotope ratios (87Sr/86Sr) point to the chemical recycling of Triassic marine evaporites. Isotope compositions (δ18O and δD) of the hydration water of gypsum point to continental waters for primary gypsum precipitation. These results are consistent with a shallow lacustrine environment for the Campo Coy gypsum depositSociedad Geológica de España20202020-01-0120202020-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/18587reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/185872026-06-02T14:58:11Z
dc.title.none.fl_str_mv The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
Los yesos del Mioceno superior de Campo Coy (Cordillera Bética oriental, España)
title The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
spellingShingle The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
Artiaga Torres, David
Evaporites
Geochemistry
Neogene Betic basins
Evaporitas
Geoquímica
Cuencas neógenas Béticas
title_short The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
title_full The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
title_fullStr The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
title_full_unstemmed The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
title_sort The late Miocene Campo Coy gypsum (Eastern Betics, Spain)
dc.creator.none.fl_str_mv Artiaga Torres, David
García Veigas, Javier
Gibert Beotas, Luis
Soria, Jesús M.
author Artiaga Torres, David
author_facet Artiaga Torres, David
García Veigas, Javier
Gibert Beotas, Luis
Soria, Jesús M.
author_role author
author2 García Veigas, Javier
Gibert Beotas, Luis
Soria, Jesús M.
author2_role author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Evaporites
Geochemistry
Neogene Betic basins
Evaporitas
Geoquímica
Cuencas neógenas Béticas
topic Evaporites
Geochemistry
Neogene Betic basins
Evaporitas
Geoquímica
Cuencas neógenas Béticas
description The Campo Coy basin contains an important evaporite succession, up to 350 meters thick of gypsum, including two gypsum units: lower and upper gypsum units. These are characterized by fine-grain laminated and selenitic primary gypsums and by nodular-laminated and meganodular secondary gypsums. The geochemical study based on sulfate isotope compositions (δ34S and δ18O) and strontium isotope ratios (87Sr/86Sr) point to the chemical recycling of Triassic marine evaporites. Isotope compositions (δ18O and δD) of the hydration water of gypsum point to continental waters for primary gypsum precipitation. These results are consistent with a shallow lacustrine environment for the Campo Coy gypsum deposit
publishDate 2020
dc.date.none.fl_str_mv 2020
2020-01-01
2020
2020-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10272/18587
url http://hdl.handle.net/10272/18587
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Sociedad Geológica de España
publisher.none.fl_str_mv Sociedad Geológica de España
dc.source.none.fl_str_mv reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname:Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15.811543

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