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Volume 29 Issue 2
Mar 2018
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Journal of Earth Science  > 2018  >  29(2): 265-279.
Shubo Li, Huiying He, Xin Qian, Yuejun Wang, Aimei Zhang. Carboniferous Arc Setting in Central Hainan: Geochronological and Geochemical Evidences on the Andesitic and Dacitic Rocks. Journal of Earth Science, 2018, 29(2): 265-279. doi: 10.1007/s12583-017-0936-0
Citation: Shubo Li, Huiying He, Xin Qian, Yuejun Wang, Aimei Zhang. Carboniferous Arc Setting in Central Hainan: Geochronological and Geochemical Evidences on the Andesitic and Dacitic Rocks. Journal of Earth Science, 2018, 29(2): 265-279. doi: 10.1007/s12583-017-0936-0
shu

Carboniferous Arc Setting in Central Hainan: Geochronological and Geochemical Evidences on the Andesitic and Dacitic Rocks

doi: 10.1007/s12583-017-0936-0
  • 1.

    Guangdong Provincial Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou 510275, China

  • 2.

    Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China

More Information
  • Corresponding author: Huiying He, hehuiy2@mail2.sysu.edu.cn
  • Received Date: 16 Jun 2017
  • Accepted Date: 05 Nov 2017
  • Publish Date: 01 Apr 2018
    Abstract
  • Volcanic rocks in the Bangxi-Chenxing tectonic zone provide important carries for better understanding the Late Paleozoic tectonic evolution in Hainan and its temporal-spatial pattern of the eastern Paleotethyan evolution. This paper presents a set of new geochronological and geochemical data on the andesitic and dacitic rocks along the Bangxi-Chenxing tectonic zone in central Hainan. The representative andesitic and dacitic samples yield similar zircon U-Pb ages of 353±3 and 351±7 Ma, respectively, being of Early Carboniferous origin. These volcanic rocks are characterized by low TiO2 and high Al2O3 contents and are enriched in LILEs and LREEs but depletion in HFSEs, along with negative εNd(t) values of -1.4– -4.7 and high 87Sr/86Sr(i) ratios of 0.707 2–0.710 1. Geochemical signatures suggest that the andesitic and dacitic samples might originate from a metasomatized wedge modified by the slab-derived component in a continental arc setting. In combination with the available data, it is proposed for the development of a Carboniferous continental arc in response to the eastern Paleotethyan evolution. The Bangxi-Chenxing tectonic zone might westerly link with the Jinshajiang-Ailaoshan-Song Ma suture zone, constituting an assemblage boundary between the South China and Indochina blocks.

     

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