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The break-up of the liassic carbonate platform in the Jabalcuz Unit (Intermediate Domain, province of Jaén)

dc.contributor.authorNieto, Luis M.
dc.contributor.authorRuiz Ortiz, Pedro Alejandro
dc.contributor.authorRey Arrans, Javier
dc.description.abstractThe break-up of the lower Liassic carbonate platform (Fm Gavilán) in the Jabalcuz area records a variety of sedimentary models of this event. Two fracture phases related to the genesis of the Fm GavUán-top unconformity have been recognized. These fracture phases and sea-level fluctuations were responsible for the differentiation of areas where, 1) condensed levels on relative submarine highs, 2) fault-related carbonate clastic wedges, and 3) paleokarst and related features on relatively more elevated and temporary emerged areas, were deposited. The presence of all this sedimentary models in a same laterally continuous outcrop, is really exceptional in the whole Betic External Zonesen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherCarbonate platformen_US
dc.subject.otherPelagic sedimentationen_US
dc.titleLa ruptura de la plataforma carbonatada Iiásica en la Unidad de Jabalcuz (dominio intermedio, prov. de Jaén)en_US
dc.titleThe break-up of the liassic carbonate platform in the Jabalcuz Unit (Intermediate Domain, province of Jaén)eng

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