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The Aptian mixed carbonate and siliciclastic ramp of Castro Urdíales (Cantabria, Northern Spain)

dc.contributor.authorRosales, Idoia
dc.contributor.authorFernández Mendiola, Pedro Ángel
dc.contributor.authorGarcía Mondéjar, Joaquín
dc.description.abstractDetailed geologic mapping and facies analysis of the Lower Aptian succession in the Castro Urdiales area led to the establishment of a mixed depositional system built of three different carbonate ramp units interlayered with two siliciclastic intraplatform trough units. Carbonate ramps characterized relative calm tectonic stages,whereas siliciclastic troughs developed during more active tectonic stages. Internally the analyzed interval contains two major sedimentary breaks, caused probably by relative sea-level falls of tectonic originen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherCarbonate rampsen_US
dc.subject.otherSiliciclastic troughsen_US
dc.subject.otherSedimentary breaksen_US
dc.subject.otherTectonic controlen_US
dc.subject.otherEarly Aptianen_US
dc.titleEl modelo de rampa mixta carbonatada y terrígena del aptiense de Castro Urdíales (Cantabria)en_US
dc.titleThe Aptian mixed carbonate and siliciclastic ramp of Castro Urdíales (Cantabria, Northern Spain)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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