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祁连褶皱系钨成矿规律研究
引用本文:高兆奎,白仲吾.祁连褶皱系钨成矿规律研究[J].甘肃地质学报,2003,12(2):59-61.
作者姓名:高兆奎  白仲吾
作者单位:甘肃省有色金属地质勘查局,甘肃省有色金属地质勘查局 甘肃兰州 730000,甘肃兰州 730000
摘    要:祁连褶皱系钨成矿与老地块密切相关,这些老地块富钨,为成矿提供了部分物质来源。大型钨矿床通常定位在NW向深断裂与NE向隐伏断裂交汇部位。加里东期的酸性侵入体对钨成矿起了决定性的作用。白钨矿矿床的形成与角闪片岩关系密切。矿区具有明显的水平分带性,中心一般为钼、铜、钨,外围为铅、锌、银。

关 键 词:钨矿  祁连褶皱系  成矿规律

STUDY ON WOLFRAM ORE-FORMING REGULARITIES OF QILIAN FOLD SYSTEM
GAO Zhao-kui and BAI Zhong-wu.STUDY ON WOLFRAM ORE-FORMING REGULARITIES OF QILIAN FOLD SYSTEM[J].Acta Geologica Gansu,2003,12(2):59-61.
Authors:GAO Zhao-kui and BAI Zhong-wu
Institution:GAO Zhao kui,BAI Zhong wu(Gansu Provincial Bureau of Geology and Exploration for Nonferrous Metals,Lanzhou 730000,China)
Abstract:The ore-formation of wolfram in Qilian fold system is closely related to the old blocks which are abundant in wolfram and provided part of wolfram for the formation of ore de- posits.Large-sized wolfram ore deposits are usually located at the area where deep faults striking northwest intersect concealed faults striking northeast.Caledonian acid intrusive rocks play a deci- sive role in the formation of wolfram ore deposits.The formation of scheelite deposit has an inti- mate relationship with amphibole-schist.The ore deposit usually has two zones,that is,W,Mo and Cu are enriched in central zone,and Pb,Zn and Ag are enriched in marginal zone
Keywords:Wolfram  Qilian fold system  Ore-forming regularities  
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