Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de "
This study evaluates a-CI-Br systematic of fluid inclusions in fluorites from "Berbes-La Cabaña" and "La Collada" districts in Asturias (N of Spain). The fluorites were formed as H20-NaCI-Ca2CI fluids represented by primary inclusions (Lwl) showing moderate salini...
| Autores: | , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 1996 |
| 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:10272/13277 |
| Acceso en línea: | http://hdl.handle.net/10272/13277 |
| Access Level: | acceso abierto |
| Palabra clave: | Fluid chemistry Fluid inclusions Fluorite Asturias |
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oai:ariasmontano.uhu.es:10272/13277 |
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Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de "Berbes-La Cabaña"y "La Collada"(Asturias)The chemistry and origin of the fluids related to the fluorites from "Berbes-La Cabaña"and La Collada"(Asturias)González Laguna, RuthBanks, D.López García, José ÁngelVindel, E.Fluid chemistryFluid inclusionsFluoriteAsturiasThis study evaluates a-CI-Br systematic of fluid inclusions in fluorites from "Berbes-La Cabaña" and "La Collada" districts in Asturias (N of Spain). The fluorites were formed as H20-NaCI-Ca2CI fluids represented by primary inclusions (Lwl) showing moderate salinity (Tm:-l 2.4° to -6.6°C) and homogenization temperature between 130° to 150°C. Lw2 inclusions are secondary with low salinity (Tm:-2.9 to -2.7°C) and global homogenization ranging between 130° to 135°C. Hypersaline Lw-s inclusions have distinguished in La Collada district. The high salinity of these inclusions could be explained as resulting of reequilibration processes. Comparison ofNa-CI-Br compositions show fundamental differences in halogen chemistry between two regions. Crush-leach extraction ana chemical analysis of the inclusions from "Berbes-La Cabaña fluorites reveals that the fluid chemistry is influenced by the fluid-rock interaction with Na-Ca exchange. The low concentration of Br suggest a brine derived from halite dissolution by reaction with evaporites. In contrast, Cl/ Br and Na/Br decrease strongly In brines from "La Collada" fluorites and are similar to modern seawater. These halogen ratios are consistent with solutes derived from evaporation of seawater.Sociedad Geológica de España19961996-01-0119961996-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/13277reponame: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:10272/132772026-06-02T14:58:11Z |
| dc.title.none.fl_str_mv |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " Berbes-La Cabaña" y " La Collada" (Asturias) The chemistry and origin of the fluids related to the fluorites from " Berbes-La Cabaña" and La Collada" (Asturias) |
| title |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " |
| spellingShingle |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " González Laguna, Ruth Fluid chemistry Fluid inclusions Fluorite Asturias |
| title_short |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " |
| title_full |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " |
| title_fullStr |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " |
| title_full_unstemmed |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " |
| title_sort |
Geoquímica y origen de los fluidos asociados a los yacimientos de fluorita de " |
| dc.creator.none.fl_str_mv |
González Laguna, Ruth Banks, D. López García, José Ángel Vindel, E. |
| author |
González Laguna, Ruth |
| author_facet |
González Laguna, Ruth Banks, D. López García, José Ángel Vindel, E. |
| author_role |
author |
| author2 |
Banks, D. López García, José Ángel Vindel, E. |
| author2_role |
author author author |
| dc.contributor.none.fl_str_mv |
|
| dc.subject.none.fl_str_mv |
Fluid chemistry Fluid inclusions Fluorite Asturias |
| topic |
Fluid chemistry Fluid inclusions Fluorite Asturias |
| description |
This study evaluates a-CI-Br systematic of fluid inclusions in fluorites from "Berbes-La Cabaña" and "La Collada" districts in Asturias (N of Spain). The fluorites were formed as H20-NaCI-Ca2CI fluids represented by primary inclusions (Lwl) showing moderate salinity (Tm:-l 2.4° to -6.6°C) and homogenization temperature between 130° to 150°C. Lw2 inclusions are secondary with low salinity (Tm:-2.9 to -2.7°C) and global homogenization ranging between 130° to 135°C. Hypersaline Lw-s inclusions have distinguished in La Collada district. The high salinity of these inclusions could be explained as resulting of reequilibration processes. Comparison ofNa-CI-Br compositions show fundamental differences in halogen chemistry between two regions. Crush-leach extraction ana chemical analysis of the inclusions from "Berbes-La Cabaña fluorites reveals that the fluid chemistry is influenced by the fluid-rock interaction with Na-Ca exchange. The low concentration of Br suggest a brine derived from halite dissolution by reaction with evaporites. In contrast, Cl/ Br and Na/Br decrease strongly In brines from "La Collada" fluorites and are similar to modern seawater. These halogen ratios are consistent with solutes derived from evaporation of seawater. |
| publishDate |
1996 |
| dc.date.none.fl_str_mv |
1996 1996-01-01 1996 1996-01-01 |
| 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/10272/13277 |
| url |
http://hdl.handle.net/10272/13277 |
| 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 |
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1869406971836235776 |
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15,812429 |