Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)

Facies distribution and sedimentary procceses in a storm dominated carbonate ramp (Kimmeridgian, northern Iberian basin) is studied in detail. Shallow ramp areas are dominated by coral reef facies. They grade basinsward into muddy facies, that have different storm deposits (storm lobes and bars, pro...

Descripción completa

Detalles Bibliográficos
Autor: Bádenas, Beatriz
Tipo de recurso: artículo
Fecha de publicación:1997
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:10272/10230
Acceso en línea:http://hdl.handle.net/10272/10230
Access Level:acceso abierto
Palabra clave:Storm deposits
Carbonate mud
Kimmeridgian ramp
Iberian basin
id ES_cd7ac730c48c698a2daef47e48bc61af
oai_identifier_str oai:ariasmontano.uhu.es:10272/10230
network_acronym_str ES
network_name_str España
repository_id_str
spelling Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)Storm deposits in a carbonate ramp: implications in the origin of the carbonate mud accumulated in distal ramp (Kimmendgian, Iberian basin)Bádenas, BeatrizStorm depositsCarbonate mudKimmeridgian rampIberian basinFacies distribution and sedimentary procceses in a storm dominated carbonate ramp (Kimmeridgian, northern Iberian basin) is studied in detail. Shallow ramp areas are dominated by coral reef facies. They grade basinsward into muddy facies, that have different storm deposits (storm lobes and bars, proximal tempestites and distal tempestites). The analysis of the relationship between these deposits along to the study of the composition of the carbonate grains, al/ow us to conclude that most of the coarse grain were produced in the reefal dominated areas. Downslope sediment transport was due to storm induced density currents. A significant part of the mud accumulated Offshore may be also resedimented in origin. Downslope transport in the studied ramp was favoured by its windward orientationSociedad Geológica de España19971997-01-0119971997-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/10230reponame: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:10272/102302026-06-02T14:58:11Z
dc.title.none.fl_str_mv Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
Storm deposits in a carbonate ramp: implications in the origin of the carbonate mud accumulated in distal ramp (Kimmendgian, Iberian basin)
title Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
spellingShingle Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
Bádenas, Beatriz
Storm deposits
Carbonate mud
Kimmeridgian ramp
Iberian basin
title_short Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
title_full Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
title_fullStr Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
title_full_unstemmed Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
title_sort Depósitos de tormenta en una rampa carbonatada: implicaciones sobre el origen del fango carbonatado acumulado en su zona distal (Kimmeridgiense, Cuenca Ibérica)
dc.creator.none.fl_str_mv Bádenas, Beatriz
author Bádenas, Beatriz
author_facet Bádenas, Beatriz
author_role author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Storm deposits
Carbonate mud
Kimmeridgian ramp
Iberian basin
topic Storm deposits
Carbonate mud
Kimmeridgian ramp
Iberian basin
description Facies distribution and sedimentary procceses in a storm dominated carbonate ramp (Kimmeridgian, northern Iberian basin) is studied in detail. Shallow ramp areas are dominated by coral reef facies. They grade basinsward into muddy facies, that have different storm deposits (storm lobes and bars, proximal tempestites and distal tempestites). The analysis of the relationship between these deposits along to the study of the composition of the carbonate grains, al/ow us to conclude that most of the coarse grain were produced in the reefal dominated areas. Downslope sediment transport was due to storm induced density currents. A significant part of the mud accumulated Offshore may be also resedimented in origin. Downslope transport in the studied ramp was favoured by its windward orientation
publishDate 1997
dc.date.none.fl_str_mv 1997
1997-01-01
1997
1997-01-01
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/10272/10230
url http://hdl.handle.net/10272/10230
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
_version_ 1869419858733563904
score 15,812455

Similares en LA Referencia