Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)

Zones of acoustic masking in sediments in the continental shelf of Cádiz, and in the Ria de Muros have been mapped utilizing 3.5 kHz and Uniboom seismic reflection records. In Cádiz the masking may be generated by shell beds, source of the shells is a Pliocene conglomerate that corresponds to the ac...

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Autor: Acosta-Yepes, Juan
Tipo de recurso: artículo
Fecha de publicación:1984
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/319929
Acceso en línea:http://hdl.handle.net/10261/319929
Access Level:acceso abierto
Palabra clave:Medio Marino
Sede Central IEO
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spelling Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)Acosta-Yepes, JuanMedio MarinoSede Central IEOZones of acoustic masking in sediments in the continental shelf of Cádiz, and in the Ria de Muros have been mapped utilizing 3.5 kHz and Uniboom seismic reflection records. In Cádiz the masking may be generated by shell beds, source of the shells is a Pliocene conglomerate that corresponds to the acoustic basement in the area. Acoustic masking in the sediments of Ria de Muros was generated by the presence of gas within the sediments. The gas is due to the decay of organic matter within the sediments. That area of acoustic masking in the Ria de Muros roughly coincides with the zone of mud with high (15.5%) organic content, and that gas bubbles were noted in the water column in the same region, support this hypothesis.Sí202320231984info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501http://hdl.handle.net/10261/319929reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésSede Central IEOhttps://www.sciencedirect.com/science/article/abs/pii/0025322784902123info:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3199292026-05-22T06:33:51Z
dc.title.none.fl_str_mv Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
title Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
spellingShingle Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
Acosta-Yepes, Juan
Medio Marino
Sede Central IEO
title_short Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
title_full Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
title_fullStr Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
title_full_unstemmed Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
title_sort Occurrence of acoustic masking in sediments in two areas of continental shelf of Spain Ria de Muros (NW) and Gulf of Cádiz (SW)
dc.creator.none.fl_str_mv Acosta-Yepes, Juan
author Acosta-Yepes, Juan
author_facet Acosta-Yepes, Juan
author_role author
dc.subject.none.fl_str_mv Medio Marino
Sede Central IEO
topic Medio Marino
Sede Central IEO
description Zones of acoustic masking in sediments in the continental shelf of Cádiz, and in the Ria de Muros have been mapped utilizing 3.5 kHz and Uniboom seismic reflection records. In Cádiz the masking may be generated by shell beds, source of the shells is a Pliocene conglomerate that corresponds to the acoustic basement in the area. Acoustic masking in the sediments of Ria de Muros was generated by the presence of gas within the sediments. The gas is due to the decay of organic matter within the sediments. That area of acoustic masking in the Ria de Muros roughly coincides with the zone of mud with high (15.5%) organic content, and that gas bubbles were noted in the water column in the same region, support this hypothesis.
publishDate 1984
dc.date.none.fl_str_mv 1984
2023
2023
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/319929
url http://hdl.handle.net/10261/319929
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Sede Central IEO
https://www.sciencedirect.com/science/article/abs/pii/0025322784902123
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
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
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