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- W2386906703 abstract "The Diaoquan deposit ,a large Ag Cu deposit, is present in the contact zone between marble and granite porphyry The ore forming process can be devided into two stages,and the country rocks show strong alteration Trace element geochemistry of rocks and sulfides suggests that the ore forming fluids are endogenic hydrothermal solutions The stable isotope studies reveal the enrichment of 34 S and show all positive values with an obvious tower effect Ore lead and biotite quartz monzonite have similar and relatively stable composition implying that they might have been derived from the lower crust Carbon and Oxygen isotopic compositions exhibit the feature of magmatic hydrothermal solutions.Inclusion thermometry gives the oreforming temperatures are of 185~400℃;salinity 40~46wt%.So it is regarded that the Diaoquan deposit is a mesothermal epithermal Ag Cu deposit.A metallogenic model has been established in this paper." @default.
- W2386906703 created "2016-06-24" @default.
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- W2386906703 date "1997-01-01" @default.
- W2386906703 modified "2023-09-22" @default.
- W2386906703 title "Geological Characteristics and Genesis of Diaoquan Silver Copper Deposit ,Shanxi Province" @default.
- W2386906703 hasPublicationYear "1997" @default.
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