Ore genesis is discussed in terms of geological features, fluid inclusions and stable isotope.The gold deposit is a magmatic hydrothermal one which was formed in the Hercynian epoch.

• 从矿床地质、流体包裹体、稳定同位素等角度较详细论述了金矿的地质特征,并进一步探讨了矿床成因,认为其属华力西早期的岩浆热液型金矿床。