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Volume 34 Issue 3
Jun 2023
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Article Contents
Journal of Earth Science  > 2023  >  34(3): 690-705.
Jie Yang, Yuansheng Du, Hu Huang, Jianghai Yang, Hongwei Huang, Zhiqiang Huang. Devonian–Carboniferous Pillow OIB-Type Basalts in the Youjiang Basin, SW China: Implications for the Eastern Extension of the Paleo-Tethys Branch Ocean. Journal of Earth Science, 2023, 34(3): 690-705. doi: 10.1007/s12583-020-1098-z
Citation: Jie Yang, Yuansheng Du, Hu Huang, Jianghai Yang, Hongwei Huang, Zhiqiang Huang. Devonian–Carboniferous Pillow OIB-Type Basalts in the Youjiang Basin, SW China: Implications for the Eastern Extension of the Paleo-Tethys Branch Ocean. Journal of Earth Science, 2023, 34(3): 690-705. doi: 10.1007/s12583-020-1098-z
shu

Devonian–Carboniferous Pillow OIB-Type Basalts in the Youjiang Basin, SW China: Implications for the Eastern Extension of the Paleo-Tethys Branch Ocean

doi: 10.1007/s12583-020-1098-z
  • 1.

    Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, School of Resources and Environment, Linyi University, Linyi 276000, China

  • 2.

    State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

  • 3.

    State Key Laboratory of Oil/Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

  • 4.

    General Academy of Geological Survey of Guangxi, Nanning 530023, China

More Information
  • Corresponding author: Yuansheng Du, duyuansheng126@126.com
  • Received Date: 22 Jul 2020
  • Accepted Date: 18 Sep 2020
    • Available Online: 08 Jun 2023
  • Issue Publish Date: 30 Jun 2023
    Abstract

  • Late Paleozoic pillow basalts are well preserved in the Youjiang Basin of SW China. In this study, we conducted geochemical and Sr-Nd isotopic study on the Late Devonian and Late Carboniferous basalts in Napo area, Youjiang Basin. The analyzed samples comprise moderate SiO2, TiO2, Mg#, and REE contents, with slightly positive or negative Eu anomalies, similar to the chemical nature of OIB (Oceanic island basalt). All basalts show low (143Nd/144Nd)i and (87Sr/86Sr)i values, close to EMI-type (Ⅰ-type Enriched Mantle) magma source. Late Carboniferous basalts display higher (87Sr/86Sr)i, Nb/Th, and lower εNd(t), Zr/Nb values than those of the Late Devonian basalts, implying progressively decreased enrichment components in the magma source processes. Such evolution trend reflects a continuous lithospheric thinning event, supporting a progressive rifting setting of the Youjiang Basin along the southwestern margin of the Yangtze Block in Late Paleozoic. Combined with regional geological background, the Youjiang Basin is viewed as a continental rift basin related to the opening of the Paleo-Tethys Ocean in Late Devonian and became a passive continental margin basin in Carboniferous. The Paleo-Tethys branch ocean probably extended further to the southern Youjiang Basin, likely corresponding to the Song Ma suture zone.

     

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