| 新疆精河县东杜斯泰铁铜矿矿床成因及找矿前景 |
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| 引用本文： | 赵强,任毅,潘志刚. 新疆精河县东杜斯泰铁铜矿矿床成因及找矿前景[J]. 资源环境与工程, 2012, 0(1): 10-13 |
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| 作者姓名： | 赵强 任毅 潘志刚 |
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| 作者单位： | 新疆维吾尔自治区地质矿产勘查开发局第七地质大队 |
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| 摘 要： | 东杜斯泰铁铜矿位于博罗科努铜金钼铅锌铁磷硫铁矿成矿带,矿床主要分布于花岗闪长岩与呼独克达坂组灰岩的接触带部位形成的矽卡岩带中,矿床赋矿岩石为矽卡岩,矿化主要为磁铁矿化、黄铜矿化、黄铁矿化、镜铁矿化、闪锌矿化,地表见少量的褐铁矿化、孔雀石化;矿区接触交代变质作用发育,围岩蚀变主要为石榴石化、绿帘石化、大理岩化、碳酸盐化;矿床成因类型为典型的矽卡岩型矿床。
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| 关 键 词： | 东杜斯泰铁铜矿 矽卡岩带 矿床成因 找矿前景 |
Ore Genesis and Prospecting Potential of East Dusitai Iron-copper Deposit in Jinghe County,Xinjiang Province |
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| ZHAO Qiang,REN Yi,PAN Zhigang. Ore Genesis and Prospecting Potential of East Dusitai Iron-copper Deposit in Jinghe County,Xinjiang Province[J]. Resources Environment & Engineering, 2012, 0(1): 10-13 |
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| Authors: | ZHAO Qiang REN Yi PAN Zhigang |
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| Affiliation: | (The 7th Brigade,Bureau of Geological Exploration & Developnent of Xinjiang,Wusu,Xinjiang 833000) |
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| Abstract: | East Dusitai iron-copper deposit is located at the Boluokenu iron-copper metallogenic belt.The deposit mainly is distributed in skarn ore belt.Skarn mineralization is mainly magnetite,chalcopyrite,pyritization,specularite and sphalerite.Meanwhile a small amount of limonitization and peacock can be seen in ground.Wallrock alteration includes garnet,epidotization petrochemical,marbleization and carbonation with the development of contact metasomatic metamorphism.Ore genesis type is typical skarn deposit. |
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| Keywords: | east Dusitai iron-copper deposit skarn ore belt ore genesis prospecting potential |
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