Plataformas carbonatadas aisladas (guyots) en el Jurásico del Subbético

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dc.contributor.authorMolina, José Miguel
dc.contributor.authorVera, J. A.
dc.date.accessioned2015-02-19T10:41:46Z
dc.date.available2015-02-19T10:41:46Z
dc.date.issued1999
dc.description.abstractIn a sector of the Southern Iberian Continental Margin (in the Median Subbetic) isolated carbonate platforms developed over volcanic edifices, forming guyots, during the middle Jurassic. In these platforms, the sedimentation started with pelagic carbonates, then calcislltites with hummocky cross-stratification were deposited and ended with oolitic bahamian limestones. These shallowing-upward sequences frequently show palaeokarstic features at the topen_US
dc.identifier.urihttp://hdl.handle.net/10272/9969
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.otherJurassicen_US
dc.subject.otherSubbeticen_US
dc.subject.otherGuyotsen_US
dc.subject.otherOolitic limestonesen_US
dc.subject.otherHummocky cross-stratificationen_US
dc.titlePlataformas carbonatadas aisladas (guyots) en el Jurásico del Subbéticoen_US
dc.titleIsolated carbonate platforms (guyots) from the Subbetic Jurassiceng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 27, (1999)