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

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

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.identifier.uri	http://hdl.handle.net/10272/16342
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.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
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	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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

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.identifier.uri	http://hdl.handle.net/10272/16342
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.language.iso	spa	es_ES
dc.publisher	Sociedad Geológica de España	es_ES
dc.rights	Atribución-NoComercial-SinDerivadas 3.0 España	*
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	info:eu-repo/semantics/article	es_ES
dc.rights.accessRights	info:eu-repo/semantics/openAccess	es_ES

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