El Albense - Cenomanense medio de la Sierra de Altomira

The Cretaceous transgression in the Sierra de Altomira starts with sandy (Utrillas Fm.) and dolomitic sediments (Villa de Ves Mb.), its detailed sequential analysis allow the recognition of five depositional sequences with a progressively less thickness from base to top: the basal sequence is terrig...

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Detalhes bibliográficos
Autores: Carenas, B., García Palacios, A., Segura, M., García Hidalgo, J. F.
Formato: artículo
Fecha de publicación:1993
País:España
Recursos:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/14027
Acesso em linha:http://hdl.handle.net/10272/14027
Access Level:acceso abierto
Palavra-chave:Depositional sequences
Albian-Cenomanian
Iberian Ranges
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spelling El Albense - Cenomanense medio de la Sierra de AltomiraThe Albian- Middle Cenomanian ofthe Altomira MountainsCarenas, B.García Palacios, A.Segura, M.García Hidalgo, J. F.Depositional sequencesAlbian-CenomanianIberian RangesThe Cretaceous transgression in the Sierra de Altomira starts with sandy (Utrillas Fm.) and dolomitic sediments (Villa de Ves Mb.), its detailed sequential analysis allow the recognition of five depositional sequences with a progressively less thickness from base to top: the basal sequence is terrigenous, appearing only in the north, it represents fluvial sediments. The second one is terrigenous in northern and southern areas, meanwhile it is dolomitic in the central area, it is interpreted as deposited in littoral environments. The 3rd and 4th sequences are composed by tidal flats dolostones. And finally, the upper sequence is composed of shallow dolostones, with a southwards decreasing thicknessesSociedad Geológica de España19931993-01-0119931993-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/14027reponame: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:10272/140272026-06-02T14:58:11Z
dc.title.none.fl_str_mv El Albense - Cenomanense medio de la Sierra de Altomira
The Albian- Middle Cenomanian ofthe Altomira Mountains
title El Albense - Cenomanense medio de la Sierra de Altomira
spellingShingle El Albense - Cenomanense medio de la Sierra de Altomira
Carenas, B.
Depositional sequences
Albian-Cenomanian
Iberian Ranges
title_short El Albense - Cenomanense medio de la Sierra de Altomira
title_full El Albense - Cenomanense medio de la Sierra de Altomira
title_fullStr El Albense - Cenomanense medio de la Sierra de Altomira
title_full_unstemmed El Albense - Cenomanense medio de la Sierra de Altomira
title_sort El Albense - Cenomanense medio de la Sierra de Altomira
dc.creator.none.fl_str_mv Carenas, B.
García Palacios, A.
Segura, M.
García Hidalgo, J. F.
author Carenas, B.
author_facet Carenas, B.
García Palacios, A.
Segura, M.
García Hidalgo, J. F.
author_role author
author2 García Palacios, A.
Segura, M.
García Hidalgo, J. F.
author2_role author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Depositional sequences
Albian-Cenomanian
Iberian Ranges
topic Depositional sequences
Albian-Cenomanian
Iberian Ranges
description The Cretaceous transgression in the Sierra de Altomira starts with sandy (Utrillas Fm.) and dolomitic sediments (Villa de Ves Mb.), its detailed sequential analysis allow the recognition of five depositional sequences with a progressively less thickness from base to top: the basal sequence is terrigenous, appearing only in the north, it represents fluvial sediments. The second one is terrigenous in northern and southern areas, meanwhile it is dolomitic in the central area, it is interpreted as deposited in littoral environments. The 3rd and 4th sequences are composed by tidal flats dolostones. And finally, the upper sequence is composed of shallow dolostones, with a southwards decreasing thicknesses
publishDate 1993
dc.date.none.fl_str_mv 1993
1993-01-01
1993
1993-01-01
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/10272/14027
url http://hdl.handle.net/10272/14027
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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score 15.812455

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