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Stratigraphy and sedimentary evolution of the upper Oxfordian-lower Tithonian in Rida (Zaragoza)

dc.contributor.authorBádenas, Beatriz
dc.contributor.authorAurell, Marc
dc.contributor.authorPérez Urresti, I.
dc.contributor.authorDelvene, G.
dc.date.accessioned2015-04-06T11:42:48Z
dc.date.available2015-04-06T11:42:48Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10235
dc.description.abstractThe Upper Jurassic of Rida consists of three depositional sequences. The HST of the lower one (Oxfordian Sequence) corresponds to the marls and marly limestone and sandstone of the lower part of the Sot de Chera Fm. The reported data and the correlation to proximaler areas of the basin allows to precise the age of the upper boundary of the sequence (topmost Planula Subbiozone,). The identification of an unconformity on top of the Rida Mb (middle part of the Loriguilla Fm) allows to differentiate two sequences (Kimmeridgian sequence-1 and Kimmeridgian sequence-2), in which the TST and the HST have been recognized. The age of the boundary between both sequences is located in the middle late Kimmeridgianen_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.otherStratigraphyen_US
dc.subject.otherUpper Jurassicen_US
dc.subject.otherIberian Basinen_US
dc.titleEstratigrafía y evolución sedimentaria del Oxfordiense superior-Titónico inferior en Riela (Zaragoza)en_US
dc.titleStratigraphy and sedimentary evolution of the upper Oxfordian-lower Tithonian in Rida (Zaragoza)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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