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- W2365366339 abstract "Sandaowanzi gold deposit is located in the southeast of Daxinganling metallogenic belt during Yanshanian epoch. It is a typical quartz vein gold deposit. Geological features, mineralizing periods, fluid inclusions and S, H, O isotope compositions are discussed to identify ore-forming source and temperature. δ~(34)S values of pyrite range from -1.1‰ to 1.7‰, showing mantle-derived sulfur character. δ~(18)O water values of ore-forming fluids responsible for quartz formation are estimated to be -15.3‰ ~ -9.9‰. δD (V-SMOW) values of inclusion fluids in quartz are measured to be -110‰ ~ -85‰. The meteoric water was dominated. Homogenization temperatures are from 181 to 267℃. The Sandaowanzi gold deposit is a mesothermal-epithermal volcanogenic gold deposit." @default.
- W2365366339 created "2016-06-24" @default.
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- W2365366339 date "2005-01-01" @default.
- W2365366339 modified "2023-09-22" @default.
- W2365366339 title "FLUID INCLUSION AND STABLE ISOTOPE GEOCHEMISTRY OF SANDAOWANZI GOLD DEPOSIT" @default.
- W2365366339 hasPublicationYear "2005" @default.
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