Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)

This work reports the timing of the rodingitization process of granitic dykes intrusive into the Ronda Peridotites. Representative fission-track ages on zircon and apatite from rodingitized dykes, in combination with cooling rates suggested for the Alpujarride Complex (Monié et al., 7 994; Sánchez-R...

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Detalhes bibliográficos
Autores: Esteban, José Julián, Cuevas, Julia, Seward, D., Tubía, José María
Tipo de documento: artigo
Data de publicação:2003
País:España
Recursos:Universidad de Huelva (UHU)
Repositório:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:inglês
OAI Identifier:oai:ariasmontano.uhu.es:10272/9090
Acesso em linha:http://hdl.handle.net/10272/9090
Access Level:Acceso aberto
Palavra-chave:Rodingíte
Fission track analysis
Cooling ages
Ronda
Betic Cordilleras
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spelling Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)Edad del proceso de rodingitización en las Peridotitas de Ronda (Cordilleras Béticas, España)Esteban, José JuliánCuevas, JuliaSeward, D.Tubía, José MaríaRodingíteFission track analysisCooling agesRondaBetic CordillerasThis work reports the timing of the rodingitization process of granitic dykes intrusive into the Ronda Peridotites. Representative fission-track ages on zircon and apatite from rodingitized dykes, in combination with cooling rates suggested for the Alpujarride Complex (Monié et al., 7 994; Sánchez-Rodrfguez, 1 998; Sosson et al., 1998) point to a minimum age of 16.8 ± 1.8 Ma for the rodingitization process. By extrapolating to the timing of formation of the highest stability limit of the serpentine minerals (500°C) we propose that the serpentinization of Ronda peridotites was a continuous process lasting at least for 2.2 Ma, from 19.1 to 16.9 Ma.Sociedad Geológica de España20032003-01-0120032003-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/9090reponame: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:10272/90902026-06-02T14:58:11Z
dc.title.none.fl_str_mv Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
Edad del proceso de rodingitización en las Peridotitas de Ronda (Cordilleras Béticas, España)
title Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
spellingShingle Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
Esteban, José Julián
Rodingíte
Fission track analysis
Cooling ages
Ronda
Betic Cordilleras
title_short Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
title_full Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
title_fullStr Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
title_full_unstemmed Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
title_sort Timing of rodingitization at the Ronda peridotites (Betic Cordilleras, Spain)
dc.creator.none.fl_str_mv Esteban, José Julián
Cuevas, Julia
Seward, D.
Tubía, José María
author Esteban, José Julián
author_facet Esteban, José Julián
Cuevas, Julia
Seward, D.
Tubía, José María
author_role author
author2 Cuevas, Julia
Seward, D.
Tubía, José María
author2_role author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Rodingíte
Fission track analysis
Cooling ages
Ronda
Betic Cordilleras
topic Rodingíte
Fission track analysis
Cooling ages
Ronda
Betic Cordilleras
description This work reports the timing of the rodingitization process of granitic dykes intrusive into the Ronda Peridotites. Representative fission-track ages on zircon and apatite from rodingitized dykes, in combination with cooling rates suggested for the Alpujarride Complex (Monié et al., 7 994; Sánchez-Rodrfguez, 1 998; Sosson et al., 1998) point to a minimum age of 16.8 ± 1.8 Ma for the rodingitization process. By extrapolating to the timing of formation of the highest stability limit of the serpentine minerals (500°C) we propose that the serpentinization of Ronda peridotites was a continuous process lasting at least for 2.2 Ma, from 19.1 to 16.9 Ma.
publishDate 2003
dc.date.none.fl_str_mv 2003
2003-01-01
2003
2003-01-01
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/10272/9090
url http://hdl.handle.net/10272/9090
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 15.81155

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