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Recognition of fossil travertine accumulations in the Aguilar Fm. (Kimmeridgian-Berriasian of Palencia and Burgos): palaeoecological and palaeohidrological implications

dc.contributor.authorHernández, José María
dc.contributor.authorDiéguez, C.
dc.contributor.authorPujalte, Victoriano
dc.contributor.authorRobles, Sergio
dc.contributor.authorWright, V. P.
dc.date.accessioned2015-04-14T08:57:04Z
dc.date.available2015-04-14T08:57:04Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10329
dc.description.abstractFossil travertine deposits have been recognized in the Aguilar Fm., which are intercalated vyithin the typical lacüstrine/palustrine limestones of this unit. Microscopically, they are characterised by numerous plant, remains and microscopically by abundant features atributáble to microbial, activity. The travertine accumulation occurred next to an important fault line that was contemporaneously active. 'Because of that; they are thought to record former hot-springs within a discharge-type water inflow systemen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherPalaeotravertineen_US
dc.subject.otherBacterial activityen_US
dc.subject.otherPalaeoecoldgy and palaeohidrologyen_US
dc.subject.otherAguilar Fm.en_US
dc.subject.otherLate jurassic-earliest Cretaceousen_US
dc.subject.otherBasquecahtabrian basinen_US
dc.titleReconocimiento de acumulaciones travertínicas fósiles en la Fm. Aguilar (Kimmeridgiense-Berriasiense de Palencia y Burgos): implicaciones paleoecológicas y paleohidrológicasen_US
dc.titleRecognition of fossil travertine accumulations in the Aguilar Fm. (Kimmeridgian-Berriasian of Palencia and Burgos): palaeoecological and palaeohidrological implicationseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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