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吉林省西林河金矿构造特征及找矿方向

STRUCTURAL FEATURES OF THE XILINHE Au DEPOSIT IN JILIN PROVINCE AND ITS PROSPECTING FOR ORES

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【作者】 赵凤桐梁宜林赵宏光徐光荣

【Author】 Zhao Fengtong Liang Yilin Zhao Hongguang Xu Guangrong(Institute of Geology and Mineral Resources,Changchun Industry Higher Specialized School,130021)

【机构】 长春工业高等专科学校矿产地质研究所

【摘要】 对矿区划分了太古宙、元古宙、中生代和新生代四个构造层;整个矿区为一棋盘格子形构造体系;主干构造形迹为由东、中、西三个韧性剪切断层群组成的间隔式泳道形韧性剪切带;成矿构造主要是三个北西韧性挤压剪切带,金矿的主要成矿构造是西部韧性挤压、剪切带,主要找矿方向为西带F_6及其派生的近南北向剪切断裂群。

【Abstract】 The mining aarea is divided into the Archean,Proterozoic, Mesozoic and Cenozoic struc-tural layers.The whole mining area exhibits a crisscross structural series,and the mian struc-tural features are interval ductile shear zones which are formed by the east-mid west-trendingductile shear-faulted groups.The metallotect feature shows mainly 3 NW ductile compres-sional shear zones.The main metallotect feature of gold deposit is a western ductile compres-sional shear zone,and mian prospecting direction for ores should be to the western F6 and tothe nearly SN shear fraulted group induced.

  • 【分类号】P618.510.2
  • 【被引频次】4
  • 【下载频次】65
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