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新疆金山沟金矿床赋存在下石炭统巴塔玛依内山组火山岩中，受火山机构的环状、放射状断裂及叠加的ＮＥ向断裂裂隙控制．蚀变发育，分为线型和面型两类蚀变带，进一步划分出成矿期前、成矿期和成矿期后３期蚀变．流体包裹体及氢、氧、碳、硫、铅同位素特征表明，参与成矿的碳为岩浆源和地层的混合碳，硫、铅来源于地幔，金等成矿元素来自火山岩，成矿溶液为大气降水与岩浆水的混合溶液．矿床成因应属浅成中低温火山岩型金矿
The Jinshangou gold deposit in Xinjiang is located in the volcanic rocks of Batamayiyishan Formation in the Lower Carboniferous. It is controlled by cyclic, radial and superimposed NE trending fracture fissures of volcanic structures. The alteration is divided into two types of alteration zones, linear and facies alteration, and further divided into three stages of alteration before the ore forming stage, the ore forming stage and the ore forming stage. The fluid inclusions and isotopic characteristics of hydrogen, oxygen, carbon, sulfur and lead show that the carbons involved in metallogenesis are mixed carbons of magmatic source and strata. Sulfur and lead are derived from mantle. Gold and other metallogenic elements are from volcanic rocks. The ore-forming solution is Atmospheric precipitation and magmatic water mixed solution. The genesis of the deposit should be shallow to medium and low temperature volcanic type gold deposit