Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga)
Holocene higstands deposits over the northern continental shelf of the Alboran Sea in the Guadalhorce river area, have been studied by means of high resolution seismic profiles and vibrocorer samples, and the high resolution stratigrahic caracterization have been carried out. These deposits develope...
| Autores: | , , , , , , |
|---|---|
| Formato: | artículo |
| Fecha de publicación: | 1996 |
| 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:10272/12170 |
| Acesso em linha: | http://hdl.handle.net/10272/12170 |
| Access Level: | acceso abierto |
| Palavra-chave: | Alboran Sea Holocene Highstand deposits Deltas Continental shelf |
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Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga)Holocene highland deposits sedimentary structure on delta of Guadalhorce River (Malaga)Fernández Salas, L. M.Hernández Molina, F. JavierSomoza, L.Villalaín, Juan JoséGuerrero, B.Alonso, J. J.Díaz del Río, VíctorAlboran SeaHoloceneHighstand depositsDeltasContinental shelfHolocene higstands deposits over the northern continental shelf of the Alboran Sea in the Guadalhorce river area, have been studied by means of high resolution seismic profiles and vibrocorer samples, and the high resolution stratigrahic caracterization have been carried out. These deposits developed constitute a thick sedimentary wedge composed of five seismic units: unit 1.- aggradational and transparente; unit 2- a weak one with an oblique-progradational configuration; unit 3- aggradational and transparent; unit 4.- a weak one with a sigmoidal-oblique progradational configuration, and unit 5.- aggradational and transparent. This structure is a consequence of two "major" relative sea levels asymmetrical cycles that took place in the Late Holocene, and were modulated at a minor scale by four sea levels cycles: a) 3600-3000 y; b) 2500-2000 & 1000-800 y; c) 400-300 y and d) 300-250 y. These minor cycles could be global and could generate asymmetrical microsequences in the sedimentary recordSociedad Geológica de España19961996-01-0119961996-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/12170reponame: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:10272/121702026-06-02T14:58:11Z |
| dc.title.none.fl_str_mv |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) Holocene highland deposits sedimentary structure on delta of Guadalhorce River (Malaga) |
| title |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) |
| spellingShingle |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) Fernández Salas, L. M. Alboran Sea Holocene Highstand deposits Deltas Continental shelf |
| title_short |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) |
| title_full |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) |
| title_fullStr |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) |
| title_full_unstemmed |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) |
| title_sort |
Estructuración sedimentaria de los depósitos de alto nivel Holoceno del delta del Rio Guadalhorce (Malaga) |
| dc.creator.none.fl_str_mv |
Fernández Salas, L. M. Hernández Molina, F. Javier Somoza, L. Villalaín, Juan José Guerrero, B. Alonso, J. J. Díaz del Río, Víctor |
| author |
Fernández Salas, L. M. |
| author_facet |
Fernández Salas, L. M. Hernández Molina, F. Javier Somoza, L. Villalaín, Juan José Guerrero, B. Alonso, J. J. Díaz del Río, Víctor |
| author_role |
author |
| author2 |
Hernández Molina, F. Javier Somoza, L. Villalaín, Juan José Guerrero, B. Alonso, J. J. Díaz del Río, Víctor |
| author2_role |
author author author author author author |
| dc.contributor.none.fl_str_mv |
|
| dc.subject.none.fl_str_mv |
Alboran Sea Holocene Highstand deposits Deltas Continental shelf |
| topic |
Alboran Sea Holocene Highstand deposits Deltas Continental shelf |
| description |
Holocene higstands deposits over the northern continental shelf of the Alboran Sea in the Guadalhorce river area, have been studied by means of high resolution seismic profiles and vibrocorer samples, and the high resolution stratigrahic caracterization have been carried out. These deposits developed constitute a thick sedimentary wedge composed of five seismic units: unit 1.- aggradational and transparente; unit 2- a weak one with an oblique-progradational configuration; unit 3- aggradational and transparent; unit 4.- a weak one with a sigmoidal-oblique progradational configuration, and unit 5.- aggradational and transparent. This structure is a consequence of two "major" relative sea levels asymmetrical cycles that took place in the Late Holocene, and were modulated at a minor scale by four sea levels cycles: a) 3600-3000 y; b) 2500-2000 & 1000-800 y; c) 400-300 y and d) 300-250 y. These minor cycles could be global and could generate asymmetrical microsequences in the sedimentary record |
| 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/10272/12170 |
| url |
http://hdl.handle.net/10272/12170 |
| 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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15,812455 |