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齐Ⅰ金矿床NW,EW向断裂构造及某地球化学特征
引用本文:刘绍忠,刘正荣,韩燕斌.齐Ⅰ金矿床NW,EW向断裂构造及某地球化学特征[J].新疆地质,1991(4).
作者姓名:刘绍忠  刘正荣  韩燕斌
作者单位:新疆维吾尔自治区地质矿产局第七地质大队 (刘绍忠,刘正荣),新疆维吾尔自治区地质矿产局第七地质大队(韩燕斌)
摘    要:本文运用多元统计分析方法,对西准齐Ⅰ金矿NW,EW向断裂构造及其地球化学特征作了初步分析研究,同时还讨论了该区断裂构造形成机制及地球化学条件.主要组合元素金、银、砷、锑、铋、汞、钨钼,即轻便共轭断裂形成的矿脉,也有其各自的最近程指示元素.结合构造条件分析,矿区内还可能存在新的隐伏矿体.

关 键 词:断裂构造  地球化学  齐Ⅰ金矿床  西准噶尔  新疆

NW AND EW TRENDING FRACTURES IN Ql-1 GOLD DEPOSIT AND THEIR GEOCHEMICAL CHARACTERISTICS
Liu Shaozhong Liu Zhenrong Han Yanbin.NW AND EW TRENDING FRACTURES IN Ql-1 GOLD DEPOSIT AND THEIR GEOCHEMICAL CHARACTERISTICS[J].Xinjiang Geology,1991(4).
Authors:Liu Shaozhong Liu Zhenrong Han Yanbin
Abstract:Multivariate Statistic Analytic Method is used in this paper not only to conduct a preliminary study of the NW and EW trending fractures in Qi-I gold deposit and their geochemical characteristic, but also to approach the mechanism and geochemical conditions of the formation of the fractures. The main indicator elements, whose association can tell much about the fractures, are Ag, As, Sb, Bi, Hg, W and Mo. Coupled with analysis of structural conditions, the above-mentioned study shows that within the ore district propably exist new blind ore bodies.
Keywords:Fracture  geochemistry  Qi-I gold deposit  western Junggar  Xinjiang
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