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Oolitic limestones between pelagic facies in the Middle Jurassic from Iznajar Cordoba province, Subbetic): palaeogeographic and palaeobathymetric significance

dc.contributor.authorVera, J. A.
dc.contributor.authorMolina, José Miguel
dc.date.accessioned2014-12-11T11:42:38Z
dc.date.available2014-12-11T11:42:38Z
dc.date.issued2001
dc.identifier.urihttp://hdl.handle.net/10272/9511
dc.description.abstractOn the top of the Zegrí Fm (Aalenian-Bajocian) oí the Median Subbetic in the Iznajar area (south of the Córdoba province) oolitic limestones outcrop, interbedded between pelagic facies. These oolitic limestones were previously interpreted as calcareous turbidites. The detailed study of their microfacies, stratigraphic location, geometry of the sedimentary beds and sedimentary structures has allowed us to interpret these limestones as deposited in isolated carbonate platforms similar to the recognized in other areas of the Median Subbetic. This interpretation asserts that the overlying and underlying pelagic sediments were deposited (o a moderate depth (some hundreds of meters)en_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherJurassicen_US
dc.subject.otherPelagic faciesen_US
dc.subject.otherOolitic limestonesen_US
dc.subject.otherHummocky cross-stratificationen_US
dc.subject.otherPalaeobathymetryen_US
dc.titleCalizas oolíticas entre facies pelágicas en el Jurásico medio de Iznájar (Prov. de Córdoba, Subbético): significado paleogeográfico y paleobati métricoen_US
dc.titleOolitic limestones between pelagic facies in the Middle Jurassic from Iznajar Cordoba province, Subbetic): palaeogeographic and palaeobathymetric significanceeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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