摘要
The salinity and density of fluid inclusions in quartz, sphalerite and calcite hosted in gold-bearing veinlets of Jianante gold deposit, Xinjiang, were studied by micro temperature measurement measurement. Also, the components in fluid inclusions were studied by using Laser Raman Spectrometry. The results indicate that ore-forming fluids are characterizd by low temperature, low salinity and low density. The conclusion is that the Jiamante Au deposit is an epithermal deposit.