Inocerámidos y sedimento carbonatado (Maastrichtiense inferior, Arco Vasco): Comportamiento de la relación 180/160 y 13C/12C durante la diagénesis. (Parte II)

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dc.contributor.authorGómez Alday, Juan José
dc.contributor.authorElorza, Javier
dc.date.accessioned2014-12-17T09:55:57Z
dc.date.available2014-12-17T09:55:57Z
dc.date.issued2001
dc.description.abstractOxygen and carbon isotopic analysis have been carried out on whole rock and inoceramid shell samples from deep-sea carbonate sediments at Sopelana II, Sopelana I and Zumaya sections (Basque Arc). The analytical results suggest that microcrystalline carbonate matrix and prismatic microstructure inoceramid shells have undergone different diagenetic paths. It is due to different isotopic mass balances which took place during fluid-carbon ate phase interaction. Under similar burial conditions, the solid phase microstructure played an important role during distribution of stable isotopes among different reservoirsen_US
dc.identifier.urihttp://hdl.handle.net/10272/9579
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherBasque Arcen_US
dc.subject.otherLower Maastrichtianen_US
dc.subject.otherInoceramidsen_US
dc.subject.otherDiagenesisen_US
dc.subject.otherSldO and 8I3C valuesen_US
dc.titleInocerámidos y sedimento carbonatado (Maastrichtiense inferior, Arco Vasco): Comportamiento de la relación 180/160 y 13C/12C durante la diagénesis. (Parte II)en_US
dc.titleInoceramids and carbonate sediment (lower Maastrichtian, Basque Arc): Behaviour of the 180/,(0 and 73C/12C ratios during diagenesis. (Part II)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 30, (2001)