Geological Characteristics and Metallogenic regularity of West Track 509 Rare Polymetallic Deposit in Dahongliutan Region, Hetian, Xinjiang
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摘要: 509道班西稀有多金属矿是在20世纪60年代发现的大红柳滩稀有金属矿基础上在外围新发现的另一处勘查基地。位于巴颜喀拉晚古生代-中生代边缘裂陷带，赋存于巴颜喀拉山群中组上段。成因类型属花岗伟晶岩型。通过对矿区地质特征、成矿规律综合研究，总结了控矿因素和找矿标志，探讨其矿床成因，经类比认为该区外围及深部有很大的找矿潜力。Abstract: The West Track 509 rare polymetallic deposit of Hetian region has been discovered in the periphery of Dahongliutan rare polymetallic deposits (that discovered in the late 1960s), which is a new polymetallic deposit exploration base. The orebody is occurred within the upper member of middle Bayankala Group in Late Palaeozoic-Mesozoic Bayankala margin rift belt. This deposit belongs to the granite pegmatite type. Through studying the geological characteristics and metallogenic regularity of this mining area, the ore-controlling factors and ore-prospecting clues of this deposit have been summarized, and its genesis has been discussed in this paper. Through contrasting research, it's found that it is benefit for enlarging prospecting in its depth and surrounding areas.
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