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- W2375399402 abstract "In this paper, four typical alkali-rich porphyry type deposits are studied by means of lead,silicon,hydrogen,oxygen,sulphur,carbon,helium and argon isotope from rockbodies and ore-veins in deposits, and the following conclusions could be obtained. The initial lead and most lead source of alkali-rich magma and silicon-rich mineralizing fluid were derived from mantle, yet it is inevitably that mantle lead mixed with some lead from crust or strata; The alkali-rich magma derived from a source in enriched mantle to be formed by mantle metasomatism is characterized by high positive number of silicon isotope composition experienced intense dynamic fractionation. But the silicon-rich mineralizing fluid, which has the nature of primary mantle, is characterized by low negative number of silicon isotope composition without dynamic fractionation. To sum up, we beliere that the mineralization was completed by silicon-rich ore-fluid auto-metasomatism to country rocks (including alkali-rich porphyry and stratum rock), and by mixing with crust rock to varying extent, during crystallization of alkali-rich magma. The silicon-rich mineralizing fluid process is a continuation of mineralization led by the mantle fluid metasomatism in crust." @default.
- W2375399402 created "2016-06-24" @default.
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- W2375399402 date "2004-01-01" @default.
- W2375399402 modified "2023-09-23" @default.
- W2375399402 title "Isotopic Geochemistry of Rock Mass and Ore-vein from Alkali-rich Porphyry Type Deposits in Western Yunnan, China" @default.
- W2375399402 hasPublicationYear "2004" @default.
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