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康山金矿产在豫西熊耳山古隆起区的结晶基底太华群和盖层中元古界熊耳群地层接触界面附近，矿体严格受构造破碎蚀变带控制。流体包裹体。稳定同位素等研究表明，成矿物质来自太华群变质岩。成矿流体的性质与变质热浪截然不同，而与花岗岩浆热波相近似。该矿床的形成与燕山期发生的同构造－花岗岩浆期热浪活动有关，金沉淀成矿阶段有大气水的混入．
The Kangshan gold deposit is controlled by tectonic crustal alteration zone in the vicinity of the contact interface between the Taihua group of the crystalline basement and the Proterozoic Xiong’er Group strata in the Xiong’ershan paleohigh uplift area in western Henan Province. Fluid inclusions. Stable isotopes and other studies have shown that the metallogenic material from Taihua Group metamorphic rocks. The nature of ore-forming fluids is quite different from that of metamorphic heat waves and similar to that of granite magma. The formation of the deposit is related to the same-tectonic-granodiorite heat wave activity occurring during the Yanshanian period, with the incorporation of atmospheric water during the gold depositional mineralization.