The rare earth element geochemistry of hydrothermal sediments from the East Pacific Rise: Examination of a seawater scavenging mechanism
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Elemental geochemical evidence for controlling factors and mechanisms of transitional organic matter accumulation: The upper Permian Longtan Formation black shale in the Lower Yangtze region, South China
2022, Journal of Natural Gas Science and EngineeringChemical characteristics of modern deep-sea metalliferous sediments in closed versus open basins, with emphasis on rare-earth elements and Nd isotopes
2021, Earth-Science ReviewsCitation Excerpt :Hence, other sources of REE must be present in the sub-lysocline sediments, for example biogenic apatite or authigenic Fe-Mn-micronodules, which as pure phases can respectively contain in the order of 5000 and 1000 ppm ∑REE (Dubinin and Sval'nov, 2001). REE data for Leg 92 sediments have been reported by Barrett et al. (1986), Ruhlin and Owen (1986) and Owen and Olivarez (1988). The new REE analyses discussed below are for a different set of samples than those given in Barrett et al. (1986).
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