La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira

A very good example of a progradational sedimentary body, the Infralittoral Prograding Wedge (IPW) has been characterized in the Algarve continental shelf developing below the storm wave base between the onshore (beach) and the offshore (inner continental shelf) depositional zones during the Late Ho...

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Detalles Bibliográficos
Autores: Hernández Molina, F. Javier, Roque, C., Lobo, Francisco J., Somoza, L., Díaz del Río, Víctor
Tipo de recurso: artículo
Fecha de publicación:1999
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:10272/9960
Acceso en línea:http://hdl.handle.net/10272/9960
Access Level:acceso abierto
Palabra clave:Gulf of Cádiz
Continental shelf
Algarve
Seismic stratigraphy
Geomorphology
Late Holocene
Highstand deposits
Infralittoral Prograding Wedge
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spelling La cuña progradante infralitoral del Holoceno Superior de Faro-TaviraLate Holocene infralittoral prograding wedge of Faro-TaviraHernández Molina, F. JavierRoque, C.Lobo, Francisco J.Somoza, L.Díaz del Río, VíctorGulf of CádizContinental shelfAlgarveSeismic stratigraphyGeomorphologyLate HoloceneHighstand depositsInfralittoral Prograding WedgeA very good example of a progradational sedimentary body, the Infralittoral Prograding Wedge (IPW) has been characterized in the Algarve continental shelf developing below the storm wave base between the onshore (beach) and the offshore (inner continental shelf) depositional zones during the Late Holocene. The main lithosome is composed of large-scale cross-beds, prograding seaward and paralleling the shoreline, which are formed by avalanches of sediments swept by waves from shallower littoral environments. Sediment transport to produce the IPW is generated by downwelling storm currents and their associated seaward bottom flowSociedad Geológica de España19991999-01-0119991999-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/9960reponame: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:10272/99602026-06-02T14:58:11Z
dc.title.none.fl_str_mv La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
Late Holocene infralittoral prograding wedge of Faro-Tavira
title La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
spellingShingle La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
Hernández Molina, F. Javier
Gulf of Cádiz
Continental shelf
Algarve
Seismic stratigraphy
Geomorphology
Late Holocene
Highstand deposits
Infralittoral Prograding Wedge
title_short La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
title_full La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
title_fullStr La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
title_full_unstemmed La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
title_sort La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira
dc.creator.none.fl_str_mv Hernández Molina, F. Javier
Roque, C.
Lobo, Francisco J.
Somoza, L.
Díaz del Río, Víctor
author Hernández Molina, F. Javier
author_facet Hernández Molina, F. Javier
Roque, C.
Lobo, Francisco J.
Somoza, L.
Díaz del Río, Víctor
author_role author
author2 Roque, C.
Lobo, Francisco J.
Somoza, L.
Díaz del Río, Víctor
author2_role author
author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Gulf of Cádiz
Continental shelf
Algarve
Seismic stratigraphy
Geomorphology
Late Holocene
Highstand deposits
Infralittoral Prograding Wedge
topic Gulf of Cádiz
Continental shelf
Algarve
Seismic stratigraphy
Geomorphology
Late Holocene
Highstand deposits
Infralittoral Prograding Wedge
description A very good example of a progradational sedimentary body, the Infralittoral Prograding Wedge (IPW) has been characterized in the Algarve continental shelf developing below the storm wave base between the onshore (beach) and the offshore (inner continental shelf) depositional zones during the Late Holocene. The main lithosome is composed of large-scale cross-beds, prograding seaward and paralleling the shoreline, which are formed by avalanches of sediments swept by waves from shallower littoral environments. Sediment transport to produce the IPW is generated by downwelling storm currents and their associated seaward bottom flow
publishDate 1999
dc.date.none.fl_str_mv 1999
1999-01-01
1999
1999-01-01
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/10272/9960
url http://hdl.handle.net/10272/9960
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 15.81155

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