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新疆多拉纳萨依金矿区构造特征与成矿关系

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王伟涛, 张复新, 张健. 新疆多拉纳萨依金矿区构造特征与成矿关系[J]. 西北地质, 2006, 39(3): 7-11.
引用本文: 王伟涛, 张复新, 张健. 新疆多拉纳萨依金矿区构造特征与成矿关系[J]. 西北地质, 2006, 39(3): 7-11.
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WANG Wei-tao, ZHANG Fu-xin, ZHANG Jian. Interrelationship of Shear Structure and Mineralizaion of Duolanasayi Gold Deposit in Xinjiang[J]. Northwestern Geology, 2006, 39(3): 7-11.
Citation: WANG Wei-tao, ZHANG Fu-xin, ZHANG Jian. Interrelationship of Shear Structure and Mineralizaion of Duolanasayi Gold Deposit in Xinjiang[J]. Northwestern Geology, 2006, 39(3): 7-11.
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新疆多拉纳萨依金矿区构造特征与成矿关系

  • 1.

    吉林大学地球科学学院, 吉林 长春 130061

  • 2.

    西北大学地质系, 陕西 西安 710069

  • 基金项目: 中国科学院创新工程项目(编号:KZC3-SW-137);国家科技攻关“305”项目(编号:2001BA609A-07-08)联合资助

Interrelationship of Shear Structure and Mineralizaion of Duolanasayi Gold Deposit in Xinjiang

  • 1.

    Institute of Geology, Jilin University, Changchun 130061, China

  • 2.

    Department of Geology, Northwest University, Xi'an 710069, China

    摘要
  • 多拉纳萨依金矿发现于20世纪80年代末,近年研究确认该矿与韧性剪切带关系密切,但对于韧性剪切带如何控制金矿床的形成并未进行深入研究。笔者从地质背景、矿床地质,以及控矿构造分析了多拉纳萨依金矿矿床特征及其成矿机理;明确了矿床产于泥盆系托克萨雷组第三岩性段的灰岩-浅变质-硅质岩系,受控于多拉纳萨依韧性剪切带;控矿构造具有二次韧性剪切变形、矿化和多期次脉体矿化的特征,显示出构造活动的多期次性与复杂性,阐明了构造期次与矿化之间的关系。
    Recent study has related the mineralizaion of Duolanasayi gold deposit (discovered in middle 1980's) to shear structures.However,how the shear structures control the gold mineralizaion is not clear.Based on the geological backg round,ore-deposit and structural geology,the paper analyzed the geological characteristics and metallogenic mechanism of the gold deposit and suggests that the deposit occurring in the limest one and metamorphic siliceous rocks in the third lithologic unit of Devonian Tuokesalei formation is controlled by the Duolanasayi shear zone characteristic of secondary shear deformation,mineralizaion and multiphased vein mineralization.These obviously show multiphase and complexity of the structural activities.
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  • 《中国矿床发现史.新疆卷》编委会.中国矿床发现史.新疆卷[M].北京:地质出版社,1996.

    芮行键,朱韶华,刘抗娟.新疆阿尔泰原生金矿基本特征及区域成矿模式[J].地质论评1993,39(2):138-148.

    李志纯,赵志忠.阿尔泰造山带和阿尔泰山构造成矿成矿域的形成[J].地质科学 2002,37(4):483-490.

    王金良.新疆阿尔泰金矿分布地质特征[J].新疆工学院学报,2000,21(3):174-177.

    李志纯.阿尔泰南缘两类构造成矿类型金矿床及其成矿模式[J].大地构造与成矿学,1999,23(1):16-40.

    沈远超,申萍,曾庆栋,刘铁兵,李光明.新疆阿尔泰金矿带主要金矿类型,成矿规律及成矿预测[J].地质与勘查 2004,40(5):1-6.

    吴富,蔡永彪.新疆多拉纳萨依金矿床地质特征和成矿机理探讨[J].新疆有色金属,2003,增刊,28-30.

    曾庆栋,沈远超,刘铁兵,李光明,申萍.新疆多拉纳萨依金矿成矿远景[J].黄金科学技术,2004,12(5):1-5.

    《China deposit discovery history.Xinjiang volume》compilers.China deposit discovery hist ory.Xinjiang volume[M].Beijing:Geology press,1996.

    Rui Xingjian,Zhushaohua,et al.Origenic gold deposit character and metallogenic modle in Altai,Xinjiang[J].Geological Review,1993,39(2):138-148.

    Li Zhichun,Zhao Zhizhong.Creation of the Altai orogenic belt and the Altai Mts teconic metallogenic province[J].geology science,2002,37(4):483:490.

    Wang Jinliang.The geological features of gold mine distribution in Alte,Xinjiang[J].Journal of Xinjiang institute of technology,2000,21(3):174-177.

    Li Zhichun.Two kinds of gold deposit and metallogenic modle on the south of margin of Altai[J].Geotectonica et metallogenia,1999,23(1):16-40.

    Shen Yuanchao,Shen Ping et al.Genetic type mineralization regulation and metallogenic prognosis of gold deposits in Altai gold ore belt,Xinjiang[J].Geology and prospection,2004,40(5):1-6.

    Wu Fu,Cai Yongbiao.Geological characteristic and metallogenic of Duolanasayi gold deposit,Xinjiang[J].Xinjiang non-ferrous metals,2003,(Sumpplement),28-30.

    Zen Qingdong,Shen Yuangchao.et al.Metallogenic perspective of Duolanasayi gold deposit,Xinjiang[J].Gold science and technology,2004,12(5):1-5

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出版历程
收稿日期:  2006-06-16
修回日期:  2006-11-22
刊出日期:  2006-09-15

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