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    中国百强科技报刊

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    Volume 46 Issue 1
    Jan.  2021
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    Article Contents
    Liu Biao, Wu Qianhong, Li Huan, Xi Xiaoshuang, Kong Hua, Cao Jingya, Jiang Jiangbo, Lin Zhiwei, Wu Jinghua, Liang Wei, 2021. Yanshanian NE-Striking Fault Evolution and Its Implications on Mineralization in the Xitian W-Sn Polymetallic Ore Field, Hunan Province. Earth Science, 46(1): 43-58. doi: 10.3799/dqkx.2019.263
    Citation: Liu Biao, Wu Qianhong, Li Huan, Xi Xiaoshuang, Kong Hua, Cao Jingya, Jiang Jiangbo, Lin Zhiwei, Wu Jinghua, Liang Wei, 2021. Yanshanian NE-Striking Fault Evolution and Its Implications on Mineralization in the Xitian W-Sn Polymetallic Ore Field, Hunan Province. Earth Science, 46(1): 43-58. doi: 10.3799/dqkx.2019.263

    Yanshanian NE-Striking Fault Evolution and Its Implications on Mineralization in the Xitian W-Sn Polymetallic Ore Field, Hunan Province

    doi: 10.3799/dqkx.2019.263
    • Received Date: 2019-10-21
    • Publish Date: 2021-01-15
    • In order to determine the fault activity history and its relationship with hydrothermal alteration and W-Sn mineralization,we investigated the field characteristics of the Yanshanian faults in the Xitian ore field and carried out microscopic identification,cathodoluminescence and ore-forming element analysis on quartz in faults. The results show that:(1) The faults are distributed in northern and southern sides of the Chahan basin and dipping to the basin,with striking directions of NE 60°-70°. High dip angles,angular breccias and pectination quartz veins in the faults indicate extensional characteristics. (2) Three stages of magmatic fluid activities occurred in the faults. The stage Ⅰ is characterized by quartz veins occurring as coarse quartz particles (0.5-15.0 mm) with local deformation and fragmentation structures. The stage Ⅱ and stage Ⅲ are typically quartz veins filling in tensile fractures with small quartz particles (0.01-2.00 mm). Moreover,stage Ⅱ quartz develops microcrack structures while stage Ⅲ quartz is idiomorphic and unreformed,suggesting a progressively weakening trend of fault deformation. (3) In contrast to stage Ⅰ and stage Ⅲ mica-free quartz veins,stage Ⅱ quartz veins involve more micas with the high contents of W and Sn elements and minor scheelites and pyrites,which show similar compositional evolutionary characteristics to that of the W-Sn deposits in the Xitian ore field. (4) The distribution of Yanshanian mineralization in the Xitian ore field is closely related to the normal faults,showing clear and regular mineralizing zonation of W-Sn and Pb-Zn deposits from the south to the north on each side of the Chahan Basin. Under the control of extensional tectonic setting of the South China Block during Yanshanian,the comprehensive extension resulting from mantle uplift and remelted magmatic intrusion may be a potential mechanism for the formation of normal faults. The extensional environment of the normal faults was favorable to accumulation of magmatic hydrothermal fluids; and the normal faults provided a channel for the migration of ore-forming hydrothermal fluids.

       

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