Zircon U-Pb Geochronological Evidence for the Evolution of the Nan-Uttaradit Suture in Northern Thailand  被引量:6

Zircon U-Pb Geochronological Evidence for the Evolution of the Nan-Uttaradit Suture in Northern Thailand

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作  者:Wenqiang Yang Xin Qian Qinglai Feng Shangyue Shen Chongpan Chonglakmani 

机构地区:[1]Wuhan Center of Geological Survey,Wuhan 430205,China [2]State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China [3]School of Earth Sciences,China University of Geosciences,Wuhan 430074,China [4]School of Geotechnology,Suranaree University of Technology,Nakhon Ratchasima 30000,Thailand

出  处:《Journal of Earth Science》2016年第3期378-390,共13页地球科学学刊(英文版)

基  金:supported by the National Natural Science Foundation of China(Nos.41172202,41190073,41302178);the China Geological Survey(No.1212011121256);the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences in Wuhan(No.MSFGPMR201402)

摘  要: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 meta- basalt, 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.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 meta- basalt, 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.

关 键 词:Nan-Uttaradit suture ophiolite mélange zircon U-Pb age northern Thailand 

分 类 号:P597.3[天文地球—地球化学] P548[天文地球—地质学]

 

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