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新疆阿克陶玛尔坎苏锰成矿带地质特征及成矿条件分析
引用本文:查斌,张连昌,张帮禄,董志国,王斌,谢志敏.新疆阿克陶玛尔坎苏锰成矿带地质特征及成矿条件分析[J].新疆地质,2019(1):75-84.
作者姓名:查斌  张连昌  张帮禄  董志国  王斌  谢志敏
作者单位:新疆维吾尔自治区地质矿产勘查开发局第二地质大队;中国科学院地质与地球物理研究所矿产资源研究重点实验室
基金项目:新疆中央返还两权价款资金项目新疆阿克陶县奥尔托喀纳什-穆呼一带锰矿调查评价(K15-2-LQ02);新疆地矿局自筹资金项目新疆西昆仑玛尔坎苏锰多金属成矿带成矿环境与靶区优选(XGMB2016007)联合资助
摘    要:玛尔坎苏锰成矿带沿玛尔坎苏河上游分布,东西延伸超过40 km。该成矿带以石炭系细碎屑岩-碳酸盐岩沉积建造为主,属典型的海相沉积型锰矿。锰矿带含矿层位稳定,矿体厚度大(最厚30.61 m),品位富(平均品位24%~35%,最高68.5%),矿石矿物以菱锰矿为主,属于低铁中磷类型。综合分析认为玛尔坎苏锰成矿带形成于滨浅海环境,成锰期处于一种安静、还原的水体环境。锰质来源以深源物质为主,与火山活动、热水活动关系密切。

关 键 词:阿克陶  玛尔坎苏  锰矿  地质特征  成矿条件

Geology Characteristic and Metallogenic Conditions of the Manganese Ore Belt in Maerkansu,Aketao,Xinjiang
Zha Bin,Zhang Lianchang,Zhang Banglu,Dong Zhiguo,Wang Bin,Xie Zhimin.Geology Characteristic and Metallogenic Conditions of the Manganese Ore Belt in Maerkansu,Aketao,Xinjiang[J].Xinjiang Geology,2019(1):75-84.
Authors:Zha Bin  Zhang Lianchang  Zhang Banglu  Dong Zhiguo  Wang Bin  Xie Zhimin
Institution:(No.2 Geological team,Xinjiang Bureau of Geology and Mineral Resources,Kashi,Xinjiang,844002,China;Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,ChineseAcademy of Sciences,Beijing,100029,China)
Abstract:In recent years,we has made a great breakthrough in the exploration of manganese ore in aketao County of Xinjiang that locates in the northwestern China,we discovered and evaluated the Maerkansu manganese ore belt.This metallogenic belt distributes along the upstream of Maerkansu River,with a length of more than 40 km from west to east. The metallogenic belt is mainly composed of the carboniferous fine clastic rock-carbonate sedimentary,Belonging to the typical marine sedimentarymanganese deposit.The metallogenic belt is stable with large thickness(Max 30.61 m) and rich grade(Average 24~35%, Max 68.5%).The ore minerals are mainly rhodochrosite and belongs to a type of lowiron with middle phosphorus;The Maerkansu manganese metallogenic belt formed in a quiet and reductive water.The main source of manganese is deep matter,which is closely related to volcanic activity and hydrothermal activity.
Keywords:Aketao  Maerkansu  Manganese deposit  Geology characteristic  Metallogenic conditions
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