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- W2363852458 abstract "The source of hydrothermal fluid and metals of deposit is very important to understand mineralization of hydrothermal sulfide on the mid-ocean ridge. He,Pb and Cu isotopic characteristics of hydrothermal sulfide from the section of ocean ridge(47°E-55°E)of Southwest Indian Ridge were analyzed,and the characteristics of mineralization sources of hydrothermal sulfide deposit were discussed.The results show that the range of N(3 He)/N(4 He)of sulfide is wide with the R/Ra of 0.85-7.02,so that the contributions of mid-ocean ridge basalt(MORB)and seawater to the sources of He are different,and the main source of He of sulfide is MORB with radiogenic He mixing partially;the ranges of Pb isotopic ratios of sulfide are limited with N(206Pb)/N(204 Pb)of 18.196-18.239,N(207 Pb)/N(204 Pb)of 15.479-15.490and N(208 Pb)/N(204Pb)of 37.951-38.023,so that compared with the wide ranges of Pb isotopic ratios of basalt from Southwest Indian Ridge,the Pb isotopes during the cycle processes of hydrothermal fluidtrend to homogeneous;the monomineral Cu isotopic compositions of sulfide are positive with the range of(0.02-0.52)×10-3,so that the characteristics of hydrothermal sulfide from Southwest Indian Ridge are heavy Cu-rich appreciably;He,Pb and Cu isotope of hydrothermal sulfide from Southwest Indian Ridge record the characteristics of hydrothermal vent fluid and source of metal,and mineralization sources of Hydrothermal Sulfide are MORB and seawater with significant recycling and late reformation of hydrothermal fluid." @default.
- W2363852458 created "2016-06-24" @default.
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- W2363852458 date "2014-01-01" @default.
- W2363852458 modified "2023-09-26" @default.
- W2363852458 title "Discussion on Sources of Metallogenic Materials of Hydrothermal Sulfide from Southwest Indian Ridge:Isotope Evidences" @default.
- W2363852458 hasPublicationYear "2014" @default.
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