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1矿床地质望峰金矿床位于乌鲁木齐市西南110km的乌鲁木齐-库尔勒公路边,大地构造上属于西天山东段的“中天山地轴”的北缘。中天山地轴以发育前寒武纪变质基底为特征,其变质变形程度明显强于南、北两侧的古生代增生带,与两侧增生带的边界断裂分别是乌瓦门断裂带和冰达坂断裂带(
1 Deposit Geological Wangfeng gold deposit is located on the edge of Urumqi-Korla Highway, 110km southwest of Urumqi, and belongs to the northern margin of the “Middle Tianshan axis” in the eastern part of the western Tianshan. The Central Tianshan axis is characterized by the development of the Precambrian metamorphic basement. The metamorphic deformation degree of the Central Tianshan Mountain is obviously stronger than that of the Paleozoic accretionary zone on both sides of the south and north sides. The boundary faults with the accretionary belts on both sides are the Wuwamen fault zone and Bingdasaka Fault zone