The analysis of H,O,C and Sr isotopes shows that this deposit is a lowtomoderate temperature volcanogene hydrothermal gold deposit in which meteoric water participates.

• 通过硫、铅、氢、氧、碳、锶等同位素及稀土元素的研究可以看出，该矿床是一个中、低温有大气水参与的火山热液型金矿床。