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通过野外考察、显微镜下薄片鉴定、X射线物相分析和矿物红外光谱等研究 ,确定了阿希金矿浊沸石化的普遍存在 ;根据浊沸石化发生的规律及其与矿床形成的关系 ,确定浊沸石化主要见于矿体的上部和外围 ,发育在地热流体系统的边缘和演化晚期 ,可作为寻找浅成低温热液型金矿的标志之一。导致阿希金矿浊沸石化的流体性质与热泉型金矿成矿流体和现代地热田类似 ,流体作用发生在石炭纪 ,证明西天山地区具有良好的浅成低温热液型金矿的形成和保存环境 ,因此找矿前景较好
Through the field investigation, the identification of thin slices under the microscope, the X-ray phase analysis and the infrared spectrum of mineral, the existence of the turbid zeolitization in the Axi gold deposit was confirmed. According to the regularity of the occurrence of turbid zeolitization and its relation with the deposit formation, Turbidite is mainly found in the upper part and the periphery of the ore body, and it is developed at the edge of the geothermal fluid system and late evolution. It can be used as one of the hallmarks of searching for epithermal gold deposits. The fluid properties that led to the turbid zeolitization of the Asi gold mine are similar to those of the hot spring-type gold mineralization fluids and the modern geothermal field, and the fluid effect occurred in the Carboniferous, proving the formation of fine epithermal gold deposits in the western Tianshan Mountains And save the environment, so prospecting is better