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- W2350449675 abstract "The characteristics of quartz in tungsten-molybdenum ore body(early mineralization stage) and fluorite fluid inclusions in lead-zinc-copper ore body(late mineralization stage),and the research of homogenization temperature and salinity of iron polymetallic deposit in Cuihongshan show that,from the early stages of tungsten-molybdenum mineralization to the late stages of lead-zinc-copper mineralization,the intrusion experienced a sharp drop of temperature and salinity significantly increased process from internal to external contact zones.The metallogenic fluid of tungsten-molybdenum ore body is magmatic hydrothermal fluids,and the metallogenic process is a single fluid cooling process.In lead-zinc-copper mineralization stage,the high temperature fluid from magma mixed with the low temperature,high salinity fluid in surrounding strata,which made the fluid temperature dropping and salinity increased,and leading to the depostion of lead,zinc,copper and other minerals.The δ34S(‰) test results of molybdenite and galena show that metallogenic materials of tungsten and molybdenum ore body mainly from the magmatic hydrothermal in internal contact zone;the metallogenic materials of lead-zinc-copper ore body in surrounding strata besides to magmatic hydrothermal origin,still may come from the leaching by rain to sulfur and other metallogenic minerals of sulfate." @default.
- W2350449675 created "2016-06-24" @default.
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- W2350449675 date "2011-01-01" @default.
- W2350449675 modified "2023-09-24" @default.
- W2350449675 title "Metallogenic fluid inclusions and sulfur isotope characteristics of Cuihongshan iron polymetallic deposit" @default.
- W2350449675 hasPublicationYear "2011" @default.
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