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dc.contributor.authorBarnolas, Antonio
dc.contributor.authorSimo, A.
dc.date.accessioned2020-07-03T15:41:32Z
dc.date.available2020-07-03T15:41:32Z
dc.date.issued1987
dc.identifier.urihttp://hdl.handle.net/10272/18424
dc.description.abstractThe oolitic succession of Middle Jurassic in age of Malorca Island is interpreted as a retrogradational base-of-slope carbonate apron sequence. The stratigraphic sequence shows oolite megabeds, oolite turbidites and hemipelagiteses_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.titleLa sedimentación oolítica del Dogger de Mallorca: Un modelo de bajada carbonática de pie de talud retrogradacionales_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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