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通过对阿克塞一步沟钨矿地质概况的简述,全面分析了钨矿床的矿化地质特征,初步认为矿床成因为在构造上与多罗尔什旋扭褶皱带有关,赋矿的岩性主要透闪石片岩、绿泥石英片岩,钨矿体物源主要来源于斜长花岗岩,赋矿岩石是距接触带有一定距离的石英片岩。区内找矿标志不太明显,主要通过夜间紫光灯照射,发亮蓝色荧光者为其直接找矿标志。找矿方向在矿区南侧与下部寻找斑岩型白钨矿床,在矿区西侧,配合1∶5万化探,继续寻找矽卡岩型与石英脉型矿床。
Based on the brief overview of the geology of the Axis Tungsten Tungsten Deposit in Axel, a comprehensive analysis of the mineralization geological features of the Tungsten Deposit is carried out. It is preliminarily believed that the ore deposit is structurally related to the Doroch spin-twist fold belt and the lithology of the ore-dressing The major tremolite, chlorite quartz schist and tungsten ore body are mainly derived from plagiogranite, and the ore-bearing rocks are quartz schist at a distance from the contact zone. Find signs of the area is not obvious, mainly through the night violet light, bright blue fluorescent for its direct ore prospecting. Prospecting direction Looking for porphyry scheelite deposits in the south and lower part of the mining area, along with 1: 50000 geochemical exploration on the west side of the mining area, continue to search for skarn-type and quartz vein-type deposits.