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    中国百强科技报刊

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    中国高校百佳科技期刊

    中国最美期刊

    Volume 43 Issue 9
    Sep.  2018
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    Article Contents
    Chen Shoubo, Huang Baoqiang, Li Chen, Tian Qinglei, Wang Chao, Wu Jianxin, Chen Mingxia, Han Jinsheng, Feng Yuzhou, Wang Yunfeng, 2018. Alteration and Mineralization of the Yuhai Cu Deposit in Eastern Tianshan, Xinjiang and Applications of Short Wavelength Infra-Red (SWIR) in Exploration. Earth Science, 43(9): 2911-2928. doi: 10.3799/dqkx.2018.156
    Citation: Chen Shoubo, Huang Baoqiang, Li Chen, Tian Qinglei, Wang Chao, Wu Jianxin, Chen Mingxia, Han Jinsheng, Feng Yuzhou, Wang Yunfeng, 2018. Alteration and Mineralization of the Yuhai Cu Deposit in Eastern Tianshan, Xinjiang and Applications of Short Wavelength Infra-Red (SWIR) in Exploration. Earth Science, 43(9): 2911-2928. doi: 10.3799/dqkx.2018.156

    Alteration and Mineralization of the Yuhai Cu Deposit in Eastern Tianshan, Xinjiang and Applications of Short Wavelength Infra-Red (SWIR) in Exploration

    doi: 10.3799/dqkx.2018.156
    • Received Date: 2018-03-17
    • Publish Date: 2018-09-15
    • The Yuhai Cu deposit, recently discovered by the No.704 Geological Party of Xinjiang Geological Exploration Bureau for Nonferrous Metals, is located in the eastern part of the Dananhu-Tousuquan island arc belt, eastern Tianshan. The alteration and mineralization features, and metallogenesis of the Yuhai deposit are still controversial. Detailed studies on ore geology, biotite and sericite Ar-Ar isotopic dating, and short wavelength infra-red (SWIR) indicate that biotite-magnetite, phyllic and chlorite alteration are well developed at Yuhai. The biotite-magnetite alteration extensively occurs in the quartz diorite, the phyllic alteration zone mainly occurs in the quartz diorite, and the chlorite alteration mainly occurs in the transitional zone of biotite-magnetite and phyllic alterations belts. Chalcopyrite mineralization occurs as chalcopyrite-pyrite-magnetite and epidote-chalcopyrite assemblages, and the former is closely related to the biotite-magnetite alteration, while the latter is associated with the phyllic alteration. The results of biotite and sericite 40Ar/39Ar dating are ca. 324-314 Ma, consistent with the age of Yuhai granite (325.4±2.5 Ma) in errors. Integrating with local geology, biotite and sericite Ar-Ar systems were likely reset after their formation. Combined with previous studies, the biotite-magnetite and phyllic alterations were likely formed at 360-350 Ma, related with the emplacement of the Yuhaixi gneissic granite (or other coeval intrusions). Short wavelength infra-red (SWIR) research at Yuhai reveals that high values (>2 253 nm) of chlorite Fe-OH absorption peak (Pos2250) mainly occur in the phyllic alteration zone and its adjacent areas, pointing to the Cu bodies, which can be used as a potential exploration tool in deposit-scale.

       

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