Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic

11 pages, 15 figures

Detalles Bibliográficos
Autores: Ercilla, Gemma, Alonso, Belén, Pérez-Belzuz, Fernando, Estrada, Ferran, Baraza, Jesús, Farran, Marcel-lí, Canals, Miquel, Masson, Douglas G.
Tipo de recurso: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:1998
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/401001
Acceso en línea:http://hdl.handle.net/10261/401001
Access Level:acceso abierto
Palabra clave:East Atlantic
Turbidite
Deposition environment
Sedimentary processes
id ES_e7880fd1c0fe4792eb2f5bf47460842f
oai_identifier_str oai:digital.csic.es:10261/401001
network_acronym_str ES
network_name_str España
repository_id_str
spelling Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern AtlanticErcilla, GemmaAlonso, BelénPérez-Belzuz, FernandoEstrada, FerranBaraza, JesúsFarran, Marcel-líCanals, MiquelMasson, Douglas G.East AtlanticTurbiditeDeposition environmentSedimentary processes11 pages, 15 figuresThe Oligocene to Recent Agadir turbidite system occurs in the Agadir Basin, abutting against the continental margin off South Morocco (central eastern Atlantic). This system is part of the submarine drainage system linking back to the Anti- and High Atlas mountains through the Agadir Canyon, and its sedimentary evolution is shown to comprise lateral shifts of canyon, channel, overbank and lobe deposits, governed by local topography (draped palaeorelief, seamounts, and a contourite ridge) and channel avulsions. In addition, the turbidite system shows an overall retrogradational stacking (migrating about 60 km upslope). This probably reflects a decrease in gradient on the continental margin, gradual basin filling, and/or a progressive decrease in energy and load of the sediment gravity flows that fed the system. The latter change in sediment flux could result from the interplay between the progressive denudation of the source areas, together with the climatic change which led to the present arid/desertic conditions in the hinterland. The seismic features observed with new ultra-high resolution seismic tools allow the recognition of the present-day sedimentary activity within the Agadir turbidite system, and this is related, among other factors, to the active seismicity of the areaPeer reviewedGeological Society of LondonConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202520251998info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionhttp://hdl.handle.net/10261/401001reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Ingléshttps://doi.org/10.1144/gsjgs.155.6.0929Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/4010012026-05-22T06:33:51Z
dc.title.none.fl_str_mv Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
title Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
spellingShingle Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
Ercilla, Gemma
East Atlantic
Turbidite
Deposition environment
Sedimentary processes
title_short Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
title_full Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
title_fullStr Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
title_full_unstemmed Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
title_sort Origin, sedimentary processes and depositional evolution of the Agadir turbidite system, central eastern Atlantic
dc.creator.none.fl_str_mv Ercilla, Gemma
Alonso, Belén
Pérez-Belzuz, Fernando
Estrada, Ferran
Baraza, Jesús
Farran, Marcel-lí
Canals, Miquel
Masson, Douglas G.
author Ercilla, Gemma
author_facet Ercilla, Gemma
Alonso, Belén
Pérez-Belzuz, Fernando
Estrada, Ferran
Baraza, Jesús
Farran, Marcel-lí
Canals, Miquel
Masson, Douglas G.
author_role author
author2 Alonso, Belén
Pérez-Belzuz, Fernando
Estrada, Ferran
Baraza, Jesús
Farran, Marcel-lí
Canals, Miquel
Masson, Douglas G.
author2_role author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv East Atlantic
Turbidite
Deposition environment
Sedimentary processes
topic East Atlantic
Turbidite
Deposition environment
Sedimentary processes
description 11 pages, 15 figures
publishDate 1998
dc.date.none.fl_str_mv 1998
2025
2025
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Postprint
info:eu-repo/semantics/acceptedVersion
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/401001
url http://hdl.handle.net/10261/401001
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv https://doi.org/10.1144/gsjgs.155.6.0929

dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Geological Society of London
publisher.none.fl_str_mv Geological Society of London
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
repository.name.fl_str_mv
repository.mail.fl_str_mv
_version_ 1869422863271854080
score 15,811543