| 哈巴河县赛都金矿成矿特征探讨 |
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| 引用本文： | 程忠富,芮行健.哈巴河县赛都金矿成矿特征探讨[J].新疆地质,1996(3). |
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| 作者姓名： | 程忠富 芮行健 |
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| 作者单位： | 中国地质科学院南京地质矿产研究所 |
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| 摘 要： | 新疆赛都金矿是属于阿尔泰地区新发现的重要金矿类型──蚀变糜棱岩型金矿。其成矿物质金主要来源于地层岩石和岩浆岩，赋矿主岩为中下泥盆统托克萨雷组的杂砂岩建造。金矿床严格受剪切构造带的控制，金矿体一般赋存于韧—脆性构造和构造扩容带中。金矿的主成矿时代为３００Ｍａ，金矿体与海西期哈巴河斜长花岗岩体存在着密切的空间—时间联系。
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| 关 键 词： | 哈巴河，赛都，蚀变糜棱岩型，金矿，剪切构造带，地层含矿性，岩浆岩，成矿时代 |
MINEROGENETIC CHARACTERISTICS OF SAIDU GOLD DEPOSIT IN HABAHE COUNTY |
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| Cheng Zhongfu, Rui Xinjian.MINEROGENETIC CHARACTERISTICS OF SAIDU GOLD DEPOSIT IN HABAHE COUNTY[J].Xinjiang Geology,1996(3). |
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| Authors: | Cheng Zhongfu Rui Xinjian |
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| Abstract: | Saidu altered-mylonite type gold deposit is an important deposit newly discovered in Habahe county of Xinjiang. It occurs in the greywacke formation of Middle-Lower Devonian Toksalei Formation. The gold deposit is totally controlled by shear structures and is formed in the ductile brittle structures and structural extension zone. The minerogenetic age of gold deposit is about 300Ma. laal gold ore body is closely related with plagioclase granites of Hercynian stage in Hahahe both in time and space. |
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| Keywords: | Habahe Saidu altered - mylonite type gold deposit shear structure zone ore-bearing property magmatite minerogenetic age |
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