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    Volume 44 Issue 9
    Sep.  2019
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    Wang Jian, Zhang Jun, Zhang Xiaojun, Liu Wenhao, Zhong Wenbin, Yang Qing, Liu Chongpeng, 2019. Rb-Sr Geochronology, Stable Isotopic Analyses and Geological Significance of the Tianbaoshan Pb-Zn Deposit in Sichuan Province, China. Earth Science, 44(9): 3026-3041. doi: 10.3799/dqkx.2018.192
    Citation: Wang Jian, Zhang Jun, Zhang Xiaojun, Liu Wenhao, Zhong Wenbin, Yang Qing, Liu Chongpeng, 2019. Rb-Sr Geochronology, Stable Isotopic Analyses and Geological Significance of the Tianbaoshan Pb-Zn Deposit in Sichuan Province, China. Earth Science, 44(9): 3026-3041. doi: 10.3799/dqkx.2018.192

    Rb-Sr Geochronology, Stable Isotopic Analyses and Geological Significance of the Tianbaoshan Pb-Zn Deposit in Sichuan Province, China

    doi: 10.3799/dqkx.2018.192
    • Received Date: 2017-10-19
    • Publish Date: 2019-09-15
    • Tianbaoshan deposit is a large Pb-Zn deposit hosted in the carbonate rocks of the Upper Sinian Dengyin Formation in Sichuan-Yunnan-Guizhou district,China. Due to the lack of accurate age data of the Pb-Zn mineralization,the related regional metallotectonic setting is still controversial. In this study,we used direct Rb-Sr chronometry of sphalerite,and combined H-O and C-O isotopic analyses to constrain the mieralizating age,the possible resources of ore-forming fluids and associated tectonic setting. An effective Rb-Sr sphalerite age of 348.5±7.2 Ma (MSWD=1.10) definitely indicates that the formation of the Tianbaoshan deposit is the Early Carboniferous. The δDH2O and δ18O values of the hydrothermal minerals (-19.3‰—-58.1‰ and 1.4‰-0.6‰,respectively) are plotted in the region of the sea water interacted with organic matter in the crustal water and the drifting to the rainwater line,indicating that the mineralizing hydrothermal fluids are mixed resources derived from interaction between seawater and organic matter of sedimentary rocks,added with meteoric water. The δ13C and δ18O values of hydrothermal calcite are divided into two different groups (-1.7‰—-1.6‰ and 12.9‰-15.2‰,and -6.5‰—-4.9‰ and 19.3‰-20.2‰,respectively),suggesting that C and O compositions of hydrothermal fluids may be derived from the dissolution of host carbonates and decarboxylation of sedimentary organic matters hosted in carbonates. The (87Sr/86Sr)i ratios of sphalerite (0.710 42±0.000 13) are higher than the those of ore-hosting carbonate rocks,whereas distinctly lower than the those of basement rocks,implying that the ore-forming material is mainly derived from the mixture of the host rocks and basement rocks. So this study highlights that there are two independent lead-zinc mineralization events in Sichuan-Yunnan-Guizhou district,in which one occurs in extensional geological environments during the Late Devonian to Early Carboniferous related to the opening of the Paleo-Tethys Ocean and the other is associated with compressional geological environments from the Late Triassic to Early Jurassic related to the closure of the Paleo-Tethys Ocean,respectively.

       

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