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通过研究新疆阿勒泰地区袄多克金矿床地质特征,结合元素地球化学剖面特征及元素组合特征分析,认为袄多克金矿床金及其他多金属元素主要赋存于中泥盆世托克萨雷组变粉砂岩、千枚岩中及顺层侵入的石英闪长岩脉中;金成矿的主要元素组合为Au-W-Bi-Ag-Pb-Zn-As;金矿属于岩浆热液后期形成的构造蚀变岩型金矿。结合区域地质背景及Au,W,Bi等元素地球化学剖面特征,认为该区具有较好的金矿成矿远景。
By studying the geological characteristics of the Duoke gold deposit in the Altay area of Xinjiang and combining the characteristics of element geochemistry and elemental assemblages, gold and other polymetallic elements in the Duoke gold deposit are mainly found in the Middle Devonian Toxale In the quartz-diorite vein in the siltstone, phyllite and phyllite intrusive layers, the main elemental composition of gold mineralization is Au-W-Bi-Ag-Pb-Zn-As; Structural alteration rock type gold deposit. Combined with regional geological background and elemental geochemical profile characteristics of Au, W, Bi, it is considered that this area has a good gold mineralization prospect.