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dc.contributor.authorPérez Mazarío, F.
dc.contributor.authorAracil Ávila, E.
dc.contributor.authorHernando, S.
dc.contributor.authorRincón, R.
dc.date.accessioned2020-06-10T11:32:12Z
dc.date.available2020-06-10T11:32:12Z
dc.date.issued1989
dc.identifier.urihttp://hdl.handle.net/10272/18251
dc.description.abstractClastic Materials of basal Muschelkalk in the northestern edge of Iberian Ranges represent subtidal environments and even high energy events in the inner platform (presence of H.C.S.). Such events disturb the inter and supratidal sedimentation development of both under and overlaying unitses_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.subject.otherMuschelkalkes_ES
dc.subject.otherIberian Rangeses_ES
dc.subject.otherTidal environmentes_ES
dc.titleLas facies terrígenas del Muschelkalk basal en el extremo noroccidental de la Cordillera Ibéricaes_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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