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- W2375280758 abstract "The systematical study of Dongtao lead-zinc deposit shows that fluid inclusions in minerals of orefield include three types:single-phase liquid inclusions(L_(H_2O)),double-phase liquid-vapor inclusions(L_(H_2O)+V_(H_2O)) and single-phase vapor inclusions(V_(H_2O)).Determination of homogenization temperatures of fluid inclusions indicates that the deposit is a low-to-moderate one with metallogenetic temperatures ranging from 90 to 355°C(usually 205-260°C), and its mineralization can be subdivided into three stages:①stratified-banded skarn lead-zinc deposit metallogenic stage,②stratoid-disseminated epidotization lead-zinc deposit metallogenic stage,③veined carbonate lead-zinc deposit metallogenic stage. Projection of salinities and homogenization temperatures shows that the mineralization depth of the deposit is 0.66-1.20 km with the salinity ranging from 7.2%-16.5%.Component analyses of the fluid inclusions indicate that the metallogenetic fluid is rich in Na~+ and poor in K~+,belonging to low-salinity NaCl-H_2O system and might be mainly derived from paleo-sea-water. Components of lead isotopes reflect that the metallogenetic materials mainly come from the crust while the δ(~(34)S) values(-6.3‰～-2.9‰)of ores indicate that sulfur is mainly from sulphate and bioaccumulation." @default.
- W2375280758 created "2016-06-24" @default.
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- W2375280758 date "2004-01-01" @default.
- W2375280758 modified "2023-09-28" @default.
- W2375280758 title "FLUID INCLUSION OF DONGTAO LEAD-ZINC DEPOSIT IN GUANGXI" @default.
- W2375280758 hasPublicationYear "2004" @default.
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