Volume 43 Issue 12
Dec.  2018
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Article Navigation >  Earth Science  > 2018  >  43(12): 4427-4442
Meng Yong, Tang Shulan, Wang Kai, Li Yanguang, 2018. Zircon U-Pb Age, Geochemistry and Tectonic Implications of Neoproterozoic Granite from South of Dabaishitou, East Tianshan. Earth Science, 43(12): 4427-4442. doi: 10.3799/dqkx.2018.174
Citation: Meng Yong, Tang Shulan, Wang Kai, Li Yanguang, 2018. Zircon U-Pb Age, Geochemistry and Tectonic Implications of Neoproterozoic Granite from South of Dabaishitou, East Tianshan. Earth Science, 43(12): 4427-4442. doi: 10.3799/dqkx.2018.174
shu

Zircon U-Pb Age, Geochemistry and Tectonic Implications of Neoproterozoic Granite from South of Dabaishitou, East Tianshan

doi: 10.3799/dqkx.2018.174
  • 1.

    Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China

  • 2.

    Orogen Research Center, China Geological Survey, Xi'an 710054, China

  • 3.

    College of Management, Xi'an University of Finance and Economics, Xi'an 710010, China

  • 4.

    School of Earth Science and Resources, Chang'an University, Xi'an 710054, China

  • Received Date: 2018-03-20
  • Publish Date: 2018-12-15
    Abstract
  • Researches on the south of Dabaishitou gneissic granite can provide constraints on early Neoproterozoic Rodinia supercontinent convergence in the East Tianshan. In this paper, zircon LA-ICP-MS U-Pb dating, in-situ Hf isotope and whole-rock geochemical composition analyses are presented for the gneissic granite. The results show that the LA-ICP-MS zircon U-Pb isotopic dating on the gneissic granite yields a mean U-Pb age of 922.7±7.9 Ma, which approximately represents the intrusive age of the granite. Geochemical characteristics of major elements of the granite exhibit high SiO2(70.04%-71.60%), Na2O+K2O(5.93%-6.58%) and Al2O3(13.88%-14.91%) contents, and low MgO(1.13%-1.29%) contents. Al2O3/TiO2(25-27) ratios are less than 100, while CaO/Na2O(0.7) and K2O/Na2O (1.6-2.2) ratios are more than 0.3 and 1.0, respectively. The gneissic granite is characterized by relative enrichment in Rb, Th, K, La, and depletion in Ba, Ta, Nb and Sr. All the samples are slightly enriched in LREE with (La/Yb)N ratios ranging from 7.29 to 8.11 (less than 10), and all the gneissic granite show clear negative Eu abnormalies (δEu < 0. 5). These characteristics are similar to values of typical S-type granite. Additionally, zircon εHf(t) values fall in the range of 3.226 78-13.727 46, with the two stage mode age from 920-1 598 Ma. Based on the chemical characteristics and Hf isotopic compositions, the Neoproterozoic gneissic granite was likely generated in a continental margin tectonic setting. With consideration of the age information on the ancient terranes from several areas, we suggest that the Tianshan ancient blocks probably formed a part of Rodinia during early Neoproterozoic period.

     

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