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

Journal of Earth Science - Tập 27 - Trang 378-390 - 2016
Wenqiang Yang1,2, Xin Qian2,3, Qinglai Feng2,3, Shangyue Shen2, Chongpan Chonglakmani4
1Wuhan Center of Geological Survey, Wuhan, China
2State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, China
3School of Earth Sciences, China University of Geosciences, Wuhan, China
4School of Geotechnology, Suranaree University of Technology, Nakhon Ratchasima, Thailand

Tóm tắt

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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