Geochemistry and Tectonic Setting of Cretaceous Sediments from Al Bauga Area, Bayuda Desert, River Nile State, Sudan

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dc.contributor.authorElzien, Hamed, B.O S.M.
dc.contributor.authorFarah, Al-Imam, O.A.O A.A
dc.contributor.authorMohamed, Kheiralla. K.M A. A
dc.contributor.authorHussein, A.H
dc.date.accessioned2018-02-01T09:38:56Z
dc.date.available2018-02-01T09:38:56Z
dc.date.issued2015-02
dc.description.abstractGeochemistry; major and trace elements of Al Bauga sediments have been investigated to understand their provenance and tectonic setting. The tectonic discriminant diagrams placed the majority of Al Bauga sediments within the passive margin setting. These sediments generally, are enrich in SiO2 and depleted in K2O and Na2O. The discriminant function diagram of major elements, the enrichment of Zr, Th, La and lack of V, Co and Ni indicate that the source area of most of Al Bauga sediments are felsic provenance.en_US
dc.identifier.issn2320-9364
dc.identifier.issn2320-9356
dc.identifier.urihttp://hdl.handle.net/123456789/10666
dc.language.isoenen_US
dc.relation.ispartofseriesInternational Journal of Research in Engineering and Science (IJRES) Vo:3;
dc.subjectGeochemistryen_US
dc.subjectmajor and trace elementsen_US
dc.subjecttectonic settingen_US
dc.subjectpassive marginen_US
dc.subjectAl Bauga sedimentsen_US
dc.titleGeochemistry and Tectonic Setting of Cretaceous Sediments from Al Bauga Area, Bayuda Desert, River Nile State, Sudanen_US
dc.typeArticleen_US

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