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对豫西熊耳山地区岩石和金矿床的铅、硫、氧和氢等同位素系统研究表明，尽管本区金矿床的类型不同，赋矿围岩性质也不尽一致，但成矿物质主要来自基底太古界太华群变质岩，成矿热液来源于燕山期花岗岩浆热液活动，金沉淀成矿阶段有大气水的混入。本区不同金矿床甚至同一矿床不同成矿阶段硫同位素组成差异的根本原因不是硫源的不同，而是受控于热液的物理化学条件及其变化。
The isotopic studies of lead, sulfur, oxygen and hydrogen in the rock and gold deposits in the Xionzaishan area, western Henan Province, show that although the types of gold deposits in this area are different and the properties of ore-hosting rocks are not consistent, the ore-forming materials mainly come from the basement The Archean Taihua Group metamorphic rocks, the ore-forming hydrothermal fluids originated from the Yanshanian granitoids magmatic hydrothermal activities, and the gold deposits were mixed with atmospheric water during the ore-forming stage. The fundamental reason for the differences in sulfur isotopic composition between different gold deposits and even the same deposit at different mineralization stages in this area is not controlled by the physical and chemical conditions of hydrothermal fluids and their changes but rather by sulfur sources.