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Volume 27 Issue 3
Jun 2016
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Wenqiang Yang, Xin Qian, Qinglai Feng, Shangyue Shen, Chongpan Chonglakmani. Zircon U-Pb geochronological evidence for the evolution of the Nan-Uttaradit suture in northern Thailand. Journal of Earth Science, 2016, 27(3): 378-390. doi: 10.1007/s12583-016-0670-z
Citation: Wenqiang Yang, Xin Qian, Qinglai Feng, Shangyue Shen, Chongpan Chonglakmani. Zircon U-Pb geochronological evidence for the evolution of the Nan-Uttaradit suture in northern Thailand. Journal of Earth Science, 2016, 27(3): 378-390. doi: 10.1007/s12583-016-0670-z

Zircon U-Pb geochronological evidence for the evolution of the Nan-Uttaradit suture in northern Thailand

doi: 10.1007/s12583-016-0670-z
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  • Corresponding author: Qinglai Feng, qinglaifeng@cug.edu.cn
  • Received Date: 07 Jun 2015
  • Accepted Date: 10 Dec 2015
  • Publish Date: 10 Jun 2016
  • The Nan-Uttaradit suture is marked by a narrow N-S trending and discontinuous ophiolite belt in northern Thailand. This suture zone is a mélange composed of gabbro, tholeiitic metabasalt, andesite and radiolarian chert. Samples of gabbro and meta-basalt in the Nan-Uttaradit suture yield zircon U-Pb ages of 311±10 and 316±3 Ma, respectively, interpreted as the crystallization ages of the rocks, suggesting the Nan-Uttaradit Ocean existed in the Late Carboniferous. Our results indicate that the Nan-Uttaradit Ocean co-existed with the Ailaoshan-Jinshajiang Ocean to the north and was probably an along-strike extension of the latter.

     

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