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甘肃滴水山金矿不同构造岩相带岩石地球化学特征及构造控矿机理探讨

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文章导航 > 西北地质 > 2018 > 51(1): 88-103

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杨永春, 刘家军, 王学银, 陈杰, 薛小文, 张聪, 任锡. 甘肃滴水山金矿不同构造岩相带岩石地球化学特征及构造控矿机理探讨[J]. 西北地质, 2018, 51(1): 88-103.
引用本文: 杨永春, 刘家军, 王学银, 陈杰, 薛小文, 张聪, 任锡. 甘肃滴水山金矿不同构造岩相带岩石地球化学特征及构造控矿机理探讨[J]. 西北地质, 2018, 51(1): 88-103.
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YANG Yongchun, LIU Jiajun, WANG Xueyin, CHEN Jie, XUE Xiaowen, ZHANG Cong, REN Xi. Geochemical Characteristics and Structural Ore-control Mechanism about Different Structural-Lithofacies Zones of the Dishuishan Gold Deposit in Gansu Province[J]. Northwestern Geology, 2018, 51(1): 88-103.
Citation: YANG Yongchun, LIU Jiajun, WANG Xueyin, CHEN Jie, XUE Xiaowen, ZHANG Cong, REN Xi. Geochemical Characteristics and Structural Ore-control Mechanism about Different Structural-Lithofacies Zones of the Dishuishan Gold Deposit in Gansu Province[J]. Northwestern Geology, 2018, 51(1): 88-103.
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甘肃滴水山金矿不同构造岩相带岩石地球化学特征及构造控矿机理探讨

  • 1.

    中国地质大学, 地质过程与矿产资源国家重点实验室, 北京 100083;甘肃省地质矿产勘查开发局第四地质矿产勘查院, 甘肃 酒泉 735000

  • 2.

    中国地质大学, 地质过程与矿产资源国家重点实验室, 北京 100083

  • 3.

    甘肃省地质矿产勘查开发局第四地质矿产勘查院, 甘肃 酒泉 735000

  • 基金项目: 国家自然科学基金重点项目“秦岭成矿域复合造山过程中印支-燕山期金-多金属成矿作用”（No.41730426）、国家自然科学基金重点项目“西秦岭卡林-类卡林型金矿床的成矿地质背景与叠加成矿作用研究”（No.41030423）、中国地质调查局“甘肃岷县寨上-马坞地区金矿整装勘查区矿产调查与找矿预测”（121201004000160901-55）联合资助

Geochemical Characteristics and Structural Ore-control Mechanism about Different Structural-Lithofacies Zones of the Dishuishan Gold Deposit in Gansu Province

  • 1.

    State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geoscience, Beijing 100083, China;Fourth Institute of Geology and Mineral Exploration of Gansu Provincial Bureau of Geology and Mineral Resources, Jiuquan 735000, Gansu, China

  • 2.

    State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Sciences and Resources, China University of Geoscience, Beijing 100083, China

  • 3.

    Fourth Institute of Geology and Mineral Exploration of Gansu Provincial Bureau of Geology and Mineral Resources, Jiuquan 735000, Gansu, China

    摘要
  • 滴水山金矿床位于北祁连加里东褶皱带的西段，分布于北西西向剪切带内，通过野外实地观察和镜下鉴定、样品测试，对该剪切带内Au2矿体构造-岩相特征及其地球化学元素变化特征进行了研究，结果表明：①该剪切带存在2期变形，早期为由北向南斜冲的韧-脆性剪切变形，晚期为斜向下滑的脆性变形。②根据元素分析结果，Au元素含量从安山质晶屑凝灰岩带→糜棱岩化安山质晶屑凝灰岩带→蚀变碎裂岩带→金矿化蚀变碎裂岩带逐步增高。根据相关性分析，Au与Ag相关性最好，其次为Pb、Mo，与As、Hg相关性一般。研究认为，滴水山金矿床北西西向剪切带早期韧-脆性变形有利于成矿元素的活化迁移，为Au元素的运移和初步富集提供了通道，晚期脆性变形主要形成各种张裂隙和构造破碎带，由于构造体制发生转换，导致Au元素的再次富集形成金矿体。
    Located at the western section of Calidonian Fold Belt in North Qilian Mountain, the Dishuishan gold deposit is distributed in NWW fault zone.The paper has studied the structural-lithofacies characteristics and its geochemical elements variation of Au2 orebody through field survey and microscopic observation and sample testing.The result show that:①There are two periods of deformation occurred in this shear zone, the early deformation is the ductile-brittle shear deformation in the process of oblique thrust from north to south, and the late deformation is brittle deformation in the process of oblique slide.②According to the results of elemental analysis, the content of gold is gradually increased from andesitic crystal tuff facie zone→ mylonitize andesitic crystal tuff facie zone→ altered cataclastec rock facie zone→ gold mineralization altered cataclastic rock facie zone, and which is significantly enriched in quartz vein.Furthermore, according to the correlation analysis, Au and Ag correlation is best, which is followed by Pb, Mo and has general correlation with the As and Hg.Research suggests that early ductile-brittle deformation in NWW fault zone is advantageous to the activation migration of ore-forming elements and provides the place for the preliminary enrichment of gold; late brittle deformation was mainly formed various tension fissure and tectonic fracture zone, with the enrichment of gold element to form gold orebodies by the transition of tectonic regime.
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出版历程
收稿日期:  2017-02-15
修回日期:  2017-11-21
刊出日期:  2018-03-15

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