| 内蒙古扎赉特旗神山铁铜矿床地质特征及找矿标志 |
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| 引用本文： | 吕骏超,刘桂香,张德宝,谭红艳,赵岩,毕中伟.内蒙古扎赉特旗神山铁铜矿床地质特征及找矿标志[J].地质与资源,2018,27(3):251-256. |
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| 作者姓名： | 吕骏超 刘桂香 张德宝 谭红艳 赵岩 毕中伟 |
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| 作者单位： | 1.中国地质调查局 沈阳地质调查中心, 辽宁 沈阳 110034;2.内蒙古自治区第六地质矿产勘查开发院, 内蒙古 海拉尔 021000 |
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| 基金项目： | 中国地质调查局项目"内蒙古扎赉特旗新林-神山地区矿产地质调查"（编号12120113055600），"大兴安岭成矿带漠河-扎兰屯地区地质矿产调查"（编号DD20160047） |
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| 摘 要： | 内蒙古神山铁铜矿床是大兴安岭重点成矿带中段具有代表性的夕卡岩型铁铜矿床.在伊力特岩体内部哲斯组残留体周边和岩体周边形成了南北两条接触带构造，其总体沿北东45~50°方向展布，北接触带东西长约1200m，南接触带东西长约3000m.矿体赋存于接触带以绿帘石-石榴子石为主的夕卡岩中，部分分布于外接触带层间剥离断层或断层中.共圈定大小矿体22条，其中主要矿体7条，单个矿体规模不大，形态复杂，矿体含铁品位较高.
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| 关 键 词： | 神山铁铜矿床 地质特征 夕卡岩型 大兴安岭中段 内蒙古 |
| 收稿时间： | 2017-03-01 |
GEOLOGICAL CHARACTERISTICS AND PROSPECTING INDICATORS OF THE SHENSHAN IRON-COPPER DEPOSIT IN JALAID QI,INNER MONGOLIA |
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| LYU Jun-chao,LIU Gui-xiang,ZHANG De-bao,TAN Hong-yan,ZHAO Yan,BI Zhong-wei.GEOLOGICAL CHARACTERISTICS AND PROSPECTING INDICATORS OF THE SHENSHAN IRON-COPPER DEPOSIT IN JALAID QI,INNER MONGOLIA[J].Geology and Resources,2018,27(3):251-256. |
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| Authors: | LYU Jun-chao LIU Gui-xiang ZHANG De-bao TAN Hong-yan ZHAO Yan BI Zhong-wei |
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| Institution: | 1.Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China;2.No. 6 Institute of Geology and Mineral Exploration and Development of Inner Mongolia, Hailar 021008, Inner Mongolia, China |
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| Abstract: | The Shenshan Fe-Cu deposit in Inner Mongolia is of typical skarn type in the middle section of Daxinganling metallogenic belt. Two contact zones from north to south occur around Yilite intrusion and the residual Zhesi formation inside the intrusion, generally distributed in NE 45-50° with lengths about 1200 m and 3000 m, respectively, from east to west. The orebodies are hosted in the skarn dominated by epidote and garnet in the contact zone, while partially distributed in faults or interlayer detachment faults of exocontact zones. Altogether 22 orebodies including 7 main orebodies are delineated with single characterized by small-scaled, complex shape and high iron content. |
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| Keywords: | Shenshan Fe-Cu deposit geological characteristics skarn type middle section of Daxinganling Mountains Inner Mongolia |
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