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以地表及钻孔岩石测量资料为基础，研究阿舍勒铜多金属矿床的原生地球化学特征，查明主要指示元素及其三度空间分布规律，建立有效的地球化学找矿评价指标。研究表明，阿舍勒矿区地层、岩石的微量元素含量显著高于成矿带和区域背景，其含量从区域→成矿带→矿区呈递增趋势；该矿床的地表原生异常沿矿化带呈“面型”展示；指示元素原生分带具有火山块状硫化物矿床上Ｚｎ下Ｃｕ的双层结构模式
Based on the surface and borehole measured data, the primary geochemical characteristics of the Ashele copper polymetallic deposit are studied, the major indicator elements and their spatial distribution patterns are ascertained three times, and an effective geochemical prospecting evaluation index is established. The results show that the content of trace elements in the strata and rocks in Ashele Mining Area is significantly higher than that in the metallogenic belt and the regional background, and the content increases from the area → the metallogenic belt → the ore area. The primary surface anomaly of the deposit shows “ Surface type ”; the primary elemental zonation of the indicator element has a double-layer structure mode with Zn under Cu on volcanic massive sulphide deposits