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- W2348651484 abstract "The study of Sr-Nd-Pb isotopic data for rocks and ores from the Laowangzhai gold deposit shows that Sr-Nd-Pb isotopic compositions are generally stable and have the same origination; high 87Sr/86Sr ratios,low 143Nd/144Nd ratios and high 206Pb/204Pb ratios of rocks and ores may be the reflection of ore-forming fluids deriving from the metasomatic enriched mantle and are mainly the result of mantle mixing with ocean sediments which are carried into mantle wedges through plate subduction. From what has been discussed above,the ore-forming fluids of the Laowangzhai gold deposit mainly derive from deep mantle,and their properties are transformed from magma fluids to hydrothermal fluids in the course of metasomatism and alteration,which leads to initiate crust-mantle mixing simultaneously to be in favor of mineralization." @default.
- W2348651484 created "2016-06-24" @default.
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- W2348651484 date "2013-01-01" @default.
- W2348651484 modified "2023-09-26" @default.
- W2348651484 title "Sr-Nd-Pb Isotopic Compositions and Their Geological Implications of the Laowangzhai Gold Deposit" @default.
- W2348651484 hasPublicationYear "2013" @default.
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