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- W2376162927 abstract "This paper studies in detail the characteristics of C, H, and O stable isotopes and primary fluid inclusions hosted in quartz and calcite from alteration samples of Guilaizhuang gold deposit in Tongshi, western Shandong. Research indicates that almost all inclusions are NaCl-H_2O solution of vapor and liquid two phases. The temperature of homogenization of the fluid inclusions ranges from 103 ℃ to 250 ℃. Ice-melting temperature varies from -2.8 ℃ to -9.3 ℃, corresponding to a range of salinities from 4.65 to 13.18 w(NaCl) equivalent. The data of stable isotopes indicate that δ~(34)S ranges from -0.71‰ to 2.990‰,δ~(13)C_(PDB) from -3.3‰ to 0.0‰,δD_(SMOW) from -48‰ to -61‰, and δ~(18)O_水 from -1.13‰ to 5.07‰ respectively. The data of δ~(34)S reveal that the ore-forming fluids originate from mantle,but those of δ~(13)C,δD_(SMOW) and δ~(18)O suggest a mixed source of mantle fluids and meteoric water. Zircon SHRIMP age suggests that the Guilaizhuang gold deposits formed in middle Jurassic epoch. Mineralization is related to cryptical blasting, pressure releasing and boiling of fluid, and deeply cyclic meteoric water mixing." @default.
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- W2376162927 date "2005-01-01" @default.
- W2376162927 modified "2023-09-25" @default.
- W2376162927 title "STUDY ON ORE-FORMING FLUIDS OF THE GUILAIZHUANG GOLD DEPOSITS IN PINGYI,WESTERN SHANDONG" @default.
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