2000
DOI: 10.1522/18320272
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Géochimie isotopique Sr-Nd-Pb des sédiments accumulés depuis 700 000 ans le long de la dorsale de Reykjanes (58-60ʻ Nord) /

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Cited by 2 publications
(6 citation statements)
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“…This allows comparisons between the different tracers and allows the detection of the main trends within the sedimentary sequence. For example, in order to test the insensitivity of neodymium to contamination of seawater, controlled attacks have been attempted on some subsamples of box-cores by partially dissolving the sample using hydrochloric acid (0.275 N HCl; Dia Hantchi, 2000). The lead was separated and purified on an ion exchange resin from an aliquot powder solution of 20 to 70 mg of dry sediment.…”
Section: Methodsmentioning
confidence: 99%
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“…This allows comparisons between the different tracers and allows the detection of the main trends within the sedimentary sequence. For example, in order to test the insensitivity of neodymium to contamination of seawater, controlled attacks have been attempted on some subsamples of box-cores by partially dissolving the sample using hydrochloric acid (0.275 N HCl; Dia Hantchi, 2000). The lead was separated and purified on an ion exchange resin from an aliquot powder solution of 20 to 70 mg of dry sediment.…”
Section: Methodsmentioning
confidence: 99%
“…This dilution would be exacerbated in the sediments of the western flank by a greater production of biogenic carbonates in this area. As, the CaCO3 content fluctuates around circa 28-46 % in the eastern flank of the Reykjanes Ridge (Savkina & al., 2018), circa 10-45 % along the axial zone and 20-80 % in the western flank of the ridge (Dia Hantchi, 2000).…”
Section: Differential Dilution Of Terrigenous Inputs By Biogenic Carbonates Vs Mixing Process Between Mantle and Crustal Materialsmentioning
confidence: 99%
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