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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.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.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherEpisodic eventses_ES
dc.subject.otherBlack shaleses_ES
dc.subject.otherStorm depositses_ES
dc.subject.otherMarine shelfes_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

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Atribución-NoComercial-SinDerivadas 3.0 España
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