Icnofósiles, sedimentación episódica/ tempestitas fangosas y «black shales» de ambientes seudoanóxicos, en sucesiones marinas de plataforma y rampa

dc.contributor.author	García Ramos, José Carlos
dc.contributor.author	Suárez de Centi, C.
dc.contributor.author	Valenzuela, M.
dc.date.accessioned	2019-06-04T09:50:52Z
dc.date.available	2019-06-04T09:50:52Z
dc.date.issued	1992
dc.description.abstract	Déposition 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 events	es_ES
dc.identifier.uri	http://hdl.handle.net/10272/16342
dc.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
dc.rights.accessRights	open access	es_ES
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/es/	*
dc.subject.other	Ichnofossils	es_ES
dc.subject.other	Episodic events	es_ES
dc.subject.other	Black shales	es_ES
dc.subject.other	Storm deposits	es_ES
dc.subject.other	Marine shelf	es_ES
dc.subject.other	Ramp	es_ES
dc.title	Icnofósiles, sedimentación episódica/ tempestitas fangosas y «black shales» de ambientes seudoanóxicos, en sucesiones marinas de plataforma y rampa	es_ES
dc.title	Ichnofossils, episodic events, mud tempestites and pseudoanoxic black shales in marine shelf and ramp successions	eng
dc.type	journal article	es_ES
dspace.entity.type	Publication

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