0904-2 < 20181210105131-914409 > on 0904-2 pub determined by oxidation of S into sulfate (Makishima et al., 2001) with HR-ICPMS Finningan, Element

measured value uncertainty unit
[S] 36.0 µg/g
tables:
  • Table 1. Major element compositions of the Horoman peridotites of Sanjeewa P. K. Malaviarachchi (2008) Highly unradiogenic lead isotope ratios from the Horoman peridotite in Japan, Nature Geoscience, 1, 859 - 863. more
  • Table 2. Trace element compositions of the Horoman samples of Sanjeewa P. K. Malaviarachchi (2008) Highly unradiogenic lead isotope ratios from the Horoman peridotite in Japan, Nature Geoscience, 1, 859 - 863. more
  • Table S2. Elemental and isotope abundances of the Horoman peridotites of Lalindra V. Ranaweera (2018) Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif, Scientific Reports, 8. more
  • Table 3. Pb isotopic composition of the Horoman samples of Sanjeewa P. K. Malaviarachchi (2008) Highly unradiogenic lead isotope ratios from the Horoman peridotite in Japan, Nature Geoscience, 1, 859 - 863. more
  • Table S3. Oxygen and lithium isotope abundances of the Horoman gabbros and Hidaka metasediments of Lalindra V. Ranaweera (2018) Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif, Scientific Reports, 8. more
  • Table S4. Results of synthetic experiments in a forsterite-water system of Lalindra V. Ranaweera (2018) Circa 1 Ga sub-seafloor hydrothermal alteration imprinted on the Horoman peridotite massif, Scientific Reports, 8. more