New discoveries of mud volcanoes on the Moroccan Atlantic continental margin (Gulf of Cádiz): morpho-structural characterization

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dc.contributor.author León Buendía, Ricardo F.
dc.contributor.author Somoza Losada, Luis
dc.contributor.author Medialdea Cela, Teresa
dc.contributor.author Vázquez, Juan Tomás
dc.contributor.author González Sanz, Francisco Javier
dc.contributor.author López-González, Nieves
dc.contributor.author Casas Layola, David
dc.contributor.author Mata Campo, Maria Pilar
dc.contributor.author Fernández Puga, María del Carmen
dc.contributor.author Giménez-Moreno, Julia
dc.contributor.author Díaz del Río, Victor
dc.date.accessioned 2020-10-02T09:31:50Z
dc.date.available 2020-10-02T09:31:50Z
dc.date.issued 2012-02-05
dc.identifier.citation Geo-Marine Letters, vol.32, n.5-6, 473–488 es_ES
dc.identifier.issn 1432-1157
dc.identifier.uri http://hdl.handle.net/20.500.12468/476
dc.description 10th International Conference on Gas in Marine Sediments, 6-11 September 2010, Listvyanka, Russia es_ES
dc.description.abstract During the MVSEIS-08 cruise of 2008, ten new mud volcanoes (MVs) were discovered on the offshore Moroccan continental margin (Gulf of Cádiz) at water depths between 750 and 1,600 m, using multibeam bathymetry, backscatter imagery, high-resolution seismic and gravity core data. Mud breccias were recovered in all cases, attesting to the nature of extrusion of these cones. The mud volcanoes are located in two fields: the MVSEIS, Moundforce, Pixie, Las Negras, Madrid, Guadix, Almanzor and El Cid MVs in the western Moroccan field, where mud volcanoes have long been suspected but to date not identified, and the Boabdil and Al Gacel MVs in the middle Moroccan field. Three main morphologies were observed: asymmetric, sub-circular and flat-topped cone-shaped types, this being the first report of asymmetric morphologies in the Gulf of Cádiz. Based on morpho-structural analysis, the features are interpreted to result from (1) repeated constructive (expulsion of fluid mud mixtures) and destructive (gravity-induced collapse and submarine landsliding) episodes and (2) interaction with bottom currents es_ES
dc.description.sponsorship División de Geología Marina, Instituto Geológico y Minero de España, España es_ES
dc.description.sponsorship Centro Oceanográfico de Málaga, Instituto Español de Oceanografía, España es_ES
dc.description.sponsorship Facultad de Ciencias del Mar, Universidad de Cádiz, España es_ES
dc.description.sponsorship Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, España es_ES
dc.language.iso en es_ES
dc.publisher Springer es_ES
dc.relation O1-LECEMA24F/ PDCTM72003/DIV/40018 es_ES
dc.relation REN2002-11669-EMAR es_ES
dc.relation CTM 2008-06399-C04/MAR es_ES
dc.rights Acceso abierto es_ES
dc.subject volcán barro es_ES
dc.subject Golfo de Cádiz es_ES
dc.subject España es_ES
dc.subject Marruecos es_ES
dc.subject margen continental es_ES
dc.subject batimetría es_ES
dc.subject retrodifusión es_ES
dc.title New discoveries of mud volcanoes on the Moroccan Atlantic continental margin (Gulf of Cádiz): morpho-structural characterization es_ES
dc.type Postprint es_ES
dc.relation.publisherversion https://link.springer.com/article/10.1007/s00367-012-0275-1 es_ES
dc.identifier.doi https://doi.org/10.1007/s00367-012-0275-1 es_ES
dc.coverage.spatialStudy España, Marruecos es_ES


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