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阿舍勒多金属矿田地质特征及Ⅰ号矿床控矿地质因素
引用本文:焦生瑞.阿舍勒多金属矿田地质特征及Ⅰ号矿床控矿地质因素[J].新疆地质,1994(4).
作者姓名:焦生瑞
作者单位:新疆维吾尔自治区地质矿产局区调管理科
摘    要:阿舍勒多金属矿田,位于阿舍勒陆缘裂陷槽中。矿田构造为两个复式向斜夹一个复式背斜组成的褶皱束,具有6组断裂,经历了3次拉张,3次闭合的演化历史。矿田地层为泥盆系火山岩建造及下石炭统火山-沉积岩建造。中泥盆世艾菲尔期和晚泥盆世弗拉斯期,为矿田的两个主要成矿期。Ⅰ号矿床形成于艾菲尔期,矿体赋存于古火山机构通道相的次辉绿岩筒筒壁间隙之中。

关 键 词:阿舍勒,多金属矿田,地质特征,古火山机构,控矿因素

GEOLOGIC CHARACTERISTICS OF ASHELE MULTIMETAL ORE FIELD AND ORE CONTROLLING FACTORS OF NO. 1 ORE DEPOSIT
Jiao Shengrui.GEOLOGIC CHARACTERISTICS OF ASHELE MULTIMETAL ORE FIELD AND ORE CONTROLLING FACTORS OF NO. 1 ORE DEPOSIT[J].Xinjiang Geology,1994(4).
Authors:Jiao Shengrui
Abstract:Ashele multimetal ore field is located at the rift depression of continental margin,characterbod by two synclinoria and one anticlinorium. The six-group fractures in the field show the evolution history of 3-time tension and 3-time closure. The stratigraphy is shown as volcanic formations of Devonian and volcanic-sedimentary formations of Lower Carboniferous. There exist two main ore mineralization stages,i. e,Aifeir stage of Middle Devonian and Feilars stage of Late Devonian. No. 1 ore deposit was formed at the Aifeir stage,with ore body mianly at the in tersetion of sub-diabade cylinder of palaeo-volcanic apparatus phase.
Keywords:Ashele  multimetal ore field  geological characteristics  palaeo-volcanic apparatus  ore-controlling factors  
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