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    Volume 34 Issue 5
    Sep.  2009
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    Article Navigation >  Earth Science  > 2009  >  34(5): 743-751
    YANG Wen-qiang, FENG Qing-lai, SHEN Shang-yue, Malila K., Chonglakmani C., 2009. Permian Radiolarians, Chert and Basalt from the Nan Suture Zone, Northern Thailand. Earth Science, 34(5): 743-751.
    Citation: YANG Wen-qiang, FENG Qing-lai, SHEN Shang-yue, Malila K., Chonglakmani C., 2009. Permian Radiolarians, Chert and Basalt from the Nan Suture Zone, Northern Thailand. Earth Science, 34(5): 743-751.
    shu

    Permian Radiolarians, Chert and Basalt from the Nan Suture Zone, Northern Thailand

    • 1.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • 2.

      School of Geotechnology, Suranaree University of Technology, Nakhon Ratchasima 30000, Thailand

    • Received Date: 2009-01-11
    • Publish Date: 2009-09-25
      Abstract
    • Well-preserved stratigraphic sequences composed of radiolarian chert and basalt were found in Pha Som metamorphic complex in Nan suture zone, northern Thailand.Bedded chert contains Follicucullus porrectus, fossils from late Middle Permian to early Late Permian.These cherts have high SiO2 (> 92.5%), low Al/ (Al+Fe+Mn) ratio (0.51 on average), and high Ce/Ce ratio (1.14 on average).These geochemical characteristics mentioned above indicate that the cherts deposited on continental margins.The basalt has high abundances of large ion lithophile elements (LILE), high field strength elements (HFSE), and light rare earth lements (LREE), suggesting characteristics of oceanic island basalt (OIB).The OIB characteristics of basalts and deep-sea-basin chert imply that the Nan suture zone was a small oceanic basin, which is similar to modern Southwest Pacific.The Nan Ocean presumably closed during the period from Late Permian to Late Triassic.

       

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