La cuña progradante infralitoral del Holoceno Superior de Faro-Tavira

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dc.contributor.authorHernández Molina, F. Javier
dc.contributor.authorRoque, C.
dc.contributor.authorLobo, Francisco J.
dc.contributor.authorSomoza, L.
dc.contributor.authorDíaz del Río, Víctor
dc.date.accessioned2015-02-18T12:44:54Z
dc.date.available2015-02-18T12:44:54Z
dc.date.issued1999
dc.description.abstractA very good example of a progradational sedimentary body, the Infralittoral Prograding Wedge (IPW) has been characterized in the Algarve continental shelf developing below the storm wave base between the onshore (beach) and the offshore (inner continental shelf) depositional zones during the Late Holocene. The main lithosome is composed of large-scale cross-beds, prograding seaward and paralleling the shoreline, which are formed by avalanches of sediments swept by waves from shallower littoral environments. Sediment transport to produce the IPW is generated by downwelling storm currents and their associated seaward bottom flowen_US
dc.identifier.urihttp://hdl.handle.net/10272/9960
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGulf of Cádizen_US
dc.subject.otherContinental shelfen_US
dc.subject.otherAlgarveen_US
dc.subject.otherSeismic stratigraphyen_US
dc.subject.otherGeomorphologyen_US
dc.subject.otherLate Holoceneen_US
dc.subject.otherHighstand depositsen_US
dc.subject.otherInfralittoral Prograding Wedgeen_US
dc.titleLa cuña progradante infralitoral del Holoceno Superior de Faro-Taviraen_US
dc.titleLate Holocene infralittoral prograding wedge of Faro-Taviraeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 27, (1999)