All Stories

  1. Abundances of Ag and Cu in mantle peridotites and the implications for the behavior of chalcophile elements in the mantle
  2. Fractionation of highly siderophile and chalcogen elements during magma transport in the mantle: Constraints from pyroxenites of the Balmuccia peridotite massif
  3. Comment on “A non-primitive origin of near-chondritic SSeTe ratios in mantle peridotites: Implications for the Earth's late accretionary history” by König S. et al. [Earth Planet. Sci. Lett. 385 (2014) 110–121]
  4. The Ore-forming Epoch of the Jiapigou Gold Belt, NE China: Evidences from the Zircon LA-ICP-MS U-Pb Dating of the Intrusive Rocks
  5. Mass Fractions of S, Cu, Se, Mo, Ag, Cd, In, Te, Ba, Sm, W, Tl and Bi in Geological Reference Materials and Selected Carbonaceous Chondrites Determined by Isotope Dilution ICP-MS
  6. Abundances of Sulfur, Selenium, Tellurium, Rhenium and Platinum-Group Elements in Eighteen Reference Materials by Isotope Dilution Sector-Field ICP-MS and Negative TIMS
  7. Multiple isotope composition (S, Pb, H, O, He, and Ar) and genetic implications for gold deposits in the Jiapigou gold belt, Northeast China
  8. Ratios of S, Se and Te in the silicate Earth require a volatile-rich late veneer
  9. Partial re-equilibration of highly siderophile elements and the chalcogens in the mantle: A case study on the Baldissero and Balmuccia peridotite massifs (Ivrea Zone, Italian Alps)
  10. Geology, Fluid Inclusion, and Sulfur Isotope Studies of the Chehugou Porphyry Molybdenum-Copper Deposit, Xilamulun Metallogenic Belt, NE China