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- W2386572644 abstract "Xindigou gold deposit occurring in the greenschist series of the Neoarchean Sertengshan Group, belongs to greenstone-type gold deposit in Daqing Mts., Inner Mongolia. Based on the (study) on the fluid-inclusion geochemistry of the ore deposit, it is suggested that the ore formed under the conditions of middle temperature(220 ～ 320 ℃),middle depth(2.8 ～ 3.8 km)and the fluid phases (separating) with the pressure decreasing. And the ore-forming fluid belongs to the Cl~--Na~+-K~+ type with low salinity(1.2 ～ 3.5 Wt%(NaCl)),and it originally derived from the magma water mixxing with meteoric water in its evolution according to the isotopes of hydrogen, oxygen (δD_(water) -67.30‰ to -98.90‰, δ~(18)O_(water) 2.662‰ to 6.985‰). And the Pb isotope and δ~(34)S of the sulfides in the ore suggest that the ore-forming substance derived from the deep part of the crust or the transitional belt between the upper mantle and lower crust." @default.
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- W2386572644 date "2004-01-01" @default.
- W2386572644 modified "2023-09-23" @default.
- W2386572644 title "The Geochemical Characteristics of Xindigou Gold Deposit, Inner Mongolia" @default.
- W2386572644 hasPublicationYear "2004" @default.
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