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    Volume 40 Issue 11
    Nov.  2015
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    Article Navigation >  Earth Science  > 2015  >  40(11): 1781-1795
    Zhang Yuzhi, Wang Yuejun, Guo Xiaofei, Gan Chengshi, Xing Xiaowan, Song Jingjing, 2015. Geochronology and Geochemistry of Cihua Neoproterozoic High-Mg Andesites in Jiangnan Orogen and Their Tectonic Implications. Earth Science, 40(11): 1781-1795. doi: 10.3799/dqkx.2015.159
    Citation: Zhang Yuzhi, Wang Yuejun, Guo Xiaofei, Gan Chengshi, Xing Xiaowan, Song Jingjing, 2015. Geochronology and Geochemistry of Cihua Neoproterozoic High-Mg Andesites in Jiangnan Orogen and Their Tectonic Implications. Earth Science, 40(11): 1781-1795. doi: 10.3799/dqkx.2015.159
    shu

    Geochronology and Geochemistry of Cihua Neoproterozoic High-Mg Andesites in Jiangnan Orogen and Their Tectonic Implications

    doi: 10.3799/dqkx.2015.159
    • 1.

      State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

    • 2.

      School of Earth Science and Geological Engineering, Sun Yat-Sen University, Guangzhou 510275, China

    • 3.

      Guangdong Provincial Key Lab of Geological Processes and Mineral Resource Survey, Guangzhou 510275, China

    • Received Date: 2015-02-09
    • Publish Date: 2015-11-15
      Abstract
    • It is generally accepted that the Jiangnan orogenic belt led to the amalgamation of the Yangtze with Cathaysia blocks during the Neoproterozoic period. However, its tectonic evolution and amalgamation timing are still in debate. This paper presents a set of new geochronological and geochemical data for the newly-identified Neoproterozoic high-Mg volcanics from Cihua (Jiangxi). LA-ICP-MS zircon U-Pb dating of the representative sample yields a weighted mean age of 832±12 Ma (n=16, MSWD=0.12), representing the eruption age of the andesite. Geochemical results indicate that they can be classified as high-Mg andesites with SiO2 ranging from 57.67% to 61.33%, MgO from 3.51% to 4.29% and Mg-number from 52 to 57. Their chondrite-normalized REE patterns exhibit a left-sloping pattern with enriched LREEs relative to HREEs. On the primitive mantle-normalized multi-element patterns, these samples have strong enrichment in LILE and depletion in HFSE with marked negative Nb-Ta, Ti and positive Th anomalies, similar to those of the typical arc volcanics. The generation of the volcanic rocks might have been attributed to an interaction of the subducted melt/fluid or sediment with the overlying refractory mantle, suggesting the central Jiangnan orogen was still on the subduction till ~832 Ma. It is concluded that the Jiangnan orogen consists of several branches with distinct amalgamation evolution.

       

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