Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar

The barite studied in the Villamayor sandstone is located in old rhizoliths related to subvertical fractures which affect these subarcosic deposits. These zones are actually in great circulation within underground waters and full of clay materials. The mineral's form together with ist miner...

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Detalles Bibliográficos
Autores: Alonso Gavilán, G., Moro Benito, M. C., Cembranos Pérez, M. L., Areas, A.
Tipo de recurso: artículo
Fecha de publicación:1997
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/10524
Acceso en línea:http://hdl.handle.net/10272/10524
Access Level:acceso abierto
Palabra clave:Barite
Neoformation
Villamayor Sandstones
Salamanca
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spelling Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminarNeoformation of barite in The Villamayor sdndslone (Salamanca). Preliminary studyAlonso Gavilán, G.Moro Benito, M. C.Cembranos Pérez, M. L.Areas, A.BariteNeoformationVillamayor SandstonesSalamancaThe barite studied in the Villamayor sandstone is located in old rhizoliths related to subvertical fractures which affect these subarcosic deposits. These zones are actually in great circulation within underground waters and full of clay materials. The mineral's form together with ist mineralogical, chemical and isotopic characteristics suggests that its formation is related with the postneogene alteration processes (caolinitization) of sandstones which liberate Ba of the feldspars and with the infiltration and circulation of metheoric waters that contain dissolved sulphatesSociedad Geológica de España19971997-01-0119971997-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/10524reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen 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:10272/105242026-06-02T14:58:11Z
dc.title.none.fl_str_mv Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
Neoformation of barite in The Villamayor sdndslone (Salamanca). Preliminary study
title Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
spellingShingle Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
Alonso Gavilán, G.
Barite
Neoformation
Villamayor Sandstones
Salamanca
title_short Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
title_full Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
title_fullStr Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
title_full_unstemmed Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
title_sort Barita de neoformación en la Arenisca de Villamayor (Salamanca). Estudio preliminar
dc.creator.none.fl_str_mv Alonso Gavilán, G.
Moro Benito, M. C.
Cembranos Pérez, M. L.
Areas, A.
author Alonso Gavilán, G.
author_facet Alonso Gavilán, G.
Moro Benito, M. C.
Cembranos Pérez, M. L.
Areas, A.
author_role author
author2 Moro Benito, M. C.
Cembranos Pérez, M. L.
Areas, A.
author2_role author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Barite
Neoformation
Villamayor Sandstones
Salamanca
topic Barite
Neoformation
Villamayor Sandstones
Salamanca
description The barite studied in the Villamayor sandstone is located in old rhizoliths related to subvertical fractures which affect these subarcosic deposits. These zones are actually in great circulation within underground waters and full of clay materials. The mineral's form together with ist mineralogical, chemical and isotopic characteristics suggests that its formation is related with the postneogene alteration processes (caolinitization) of sandstones which liberate Ba of the feldspars and with the infiltration and circulation of metheoric waters that contain dissolved sulphates
publishDate 1997
dc.date.none.fl_str_mv 1997
1997-01-01
1997
1997-01-01
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/10272/10524
url http://hdl.handle.net/10272/10524
dc.language.none.fl_str_mv Español
spa
language_invalid_str_mv Español
language spa
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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