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希勒库都克为近年来发现的一个以钼为主的铜钼矿床.在对矿床地质背景、矿区地质特征、矿体和矿石特征、矿化阶段和分带、围岩蚀变及矿床地球化学研究基础上,认为希勒库都克矿床以铜-钼组合、细脉浸染状矿化为特征,成矿与中酸性(次火山)斑岩脉有关,围岩蚀变具斑岩矿床的分带特征.成矿物质来自含矿斑岩,成矿流体来自岩浆水和天水混合.成矿温度和盐度较高,属斑岩铜钼矿床成因.辉钼矿Re-Os等时线年龄为(327.1±2.9)Ma.进一步研究表明,该矿床含矿斑岩锆石U-Pb年龄为(329.2±8.2)Ma,SiO2在70.37%～73.46%,K2O在3.65%～3.96%,铝饱和指数(A/CNK)为0.99~1.03,σ为1.48～1.87,属弱过铝质高钾钙碱性系列岩石.矿床产于后碰撞构造环境,在新疆北部这类斑岩铜钼矿床具良好的找矿潜力.
Hiluxuoduke is a molybdenum-based copper-molybdenum deposit discovered in recent years.After studying the geological background of the deposit, geological characteristics of the mining area, characteristics of ore body and ore, mineralization stage and zoning, wall rock alteration and deposit earth On the basis of chemical research, it is considered that the Hilletukurk deposit is characterized by copper-molybdenum assemblage and disseminated disseminated mineralization. The mineralization is related to moderately acidic (subvolcanic) porphyry veins, The ore-forming materials come from ore-bearing porphyries, and the ore-forming fluids come from the mixing of magma water and Tianshui.The ore-forming temperature and salinity are higher and belong to the porphyry copper-molybdenum deposit.The Re-Os isochron age of molybdenite (327.1 ± 2.9) Ma. Further studies indicate that the U-Pb zircon age of the ore-bearing porphyries in this deposit is (329.2 ± 8.2) Ma, with SiO2 in the range of 70.37% ~ 73.46%, K2O in 3.65% ~ 3.96% The index (A / CNK) is 0.99 ~ 1.03 and σ is 1.48-1.87, which belongs to the weak permanganic high-K calc-alkaline series rocks.The orebodies are produced in post-collision tectonic setting, and the porphyry Cu and Mo deposits in northern Xinjiang are well- Prospecting potential.