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dc.contributor.authorBarnolas, Antonio
dc.contributor.authorSimo, A.
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.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.titleLa sedimentación oolítica del Dogger de Mallorca: Un modelo de bajada carbonática de pie de talud retrogradacionales_ES

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Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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