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Bioturbate structures of the Muschelka lk fades in the Subbetic Zone

dc.contributor.authorPérez López, Alberto
dc.date.accessioned2019-06-03T11:42:38Z
dc.date.available2019-06-03T11:42:38Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/16338
dc.description.abstractIn Majanillos Formation (middle -upper Ladinian age) of the Subbetic Zone, the bioturbate textures are related with deep ramp facies. F/ieTlialassinoides trace fossil is placed in the middle levels of the formation corresponding to lagoon facies (low energy). And the Diplocaaterion, Rhizocorallium and Chondrites trace fossils are related with the shallower facies of a restricted stonees_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.otherTriassices_ES
dc.subject.otherMuschelkalkes_ES
dc.subject.otherSubbetices_ES
dc.subject.otherTrace fossiles_ES
dc.titleEstructuras bioturbadas de las facies Muschelkalk de la Zona Subbéticaes_ES
dc.titleBioturbate structures of the Muschelka lk fades in the Subbetic Zoneeng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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