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      Data report: X-ray florescence scanning of sediment cores, Site U1419, Gulf of Alaska: Expedition 341

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      Proceedings of the IODP
      Integrated Ocean Drilling Program

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          Abstract

          Semiquantitative elemental results from X-ray fluorescence (XRF) scanning of sediment cores from Integrated Ocean Drilling Program (IODP) Site U1419 in the Gulf of Alaska are presented. This site contains varying lithofacies that have been previously correlated with glacial–interglacial changes in sedimentation and water-column productivity. XRF scanning was conducted to aid in interpretation of sedimentation during the last glacial period.

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          Composition of the Continental Crust

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            Influence of the water content on X-ray fluorescence core-scanning measurements in soft marine sediments

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              The Avaatech XRF Core Scanner: technical description and applications to NE Atlantic sediments

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                Author and article information

                Journal
                10.2204/iodp.proc.341.2014
                Proceedings of the IODP
                Integrated Ocean Drilling Program
                1930-1014
                21 July 2017
                Article
                10.2204/iodp.proc.341.203.2017
                67123721-bd4c-41a4-a7d6-990b8e80ad1a

                This work is licensed under a Creative Commons Attribution 4.0 Unported License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

                History

                Earth & Environmental sciences,Oceanography & Hydrology,Geophysics,Chemistry,Geosciences

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