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Meaning of the bioturbations in a continental evaporitic environment (Miocene of the Madrid Basin)

dc.contributor.authorRodríguez Aranda, J. Pablo
dc.date.accessioned2019-06-12T10:06:47Z
dc.date.available2019-06-12T10:06:47Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/16401
dc.description.abstractSeveral types of bioturbation traces have been recognized within sedimentary deposits belonging to the Miocene Lower and Intermediate Units of the Eastern part of the Madrid Basin. The bioturbation traces are developed in muddy, carbonate and gypsiferous deposits that are interpreted as mudflat, ephemeral ponds and brackishto-saline lake facies. The bioturbation traces, whether caused by roots or meiofauna, inform about the depositional paleoenvironment. On the other hand, they influence both depositional and diagenetic fabricses_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.otherMudflates_ES
dc.subject.otherSaline lakees_ES
dc.subject.otherBioturbationes_ES
dc.subject.otherDiagenesises_ES
dc.subject.otherMadrid Basines_ES
dc.titleSignificado de bioturbaciones en un medio evaporítico continental (Mioceno de la Cuenca de Madrid)es_ES
dc.titleMeaning of the bioturbations in a continental evaporitic environment (Miocene of the Madrid Basin)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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