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Ichnofossils, episodic events, mud tempestites and pseudoanoxic black shales in marine shelf and ramp successions

dc.contributor.authorGarcía Ramos, José Carlos
dc.contributor.authorSuárez de Centi, C.
dc.contributor.authorValenzuela, M.
dc.date.accessioned2019-06-04T09:50:52Z
dc.date.available2019-06-04T09:50:52Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/10272/16342
dc.description.abstractDéposition of blade shale fades on marine shelves and ramps has been habitually attributed to several causes related to oxygen-depleted bottom waters: sea level fluctuations, very slow water circulation, high organic productivity in the surface water; etc. This paper concerns to black shale deposits quickly accumulated on a w e ll oxygenated bottom, devoid o f bioturbation, and related to mud-rich storm eventses_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.otherIchnofossilses_ES
dc.subject.otherEpisodic eventses_ES
dc.subject.otherBlack shaleses_ES
dc.subject.otherStorm depositses_ES
dc.subject.otherMarine shelfes_ES
dc.subject.otherRampes_ES
dc.titleIcnofósiles, sedimentación episódica/ tempestitas fangosas y «black shales» de ambientes seudoanóxicos, en sucesiones marinas de plataforma y rampaes_ES
dc.titleIchnofossils, episodic events, mud tempestites and pseudoanoxic black shales in marine shelf and ramp successionseng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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