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《Chinese Geology》 2004-03
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Dating of gabbro in the Shemalagou ophiolite in the westernsegment of the Bangong Co-Nujiang ophiolite belt, Tibet-with a discussion of the age of the Bangong Co-Nujiang ophiolite belt

QIU Rui-zhao1, ZHOU Su2,3, DENG Jin-fu3, LI Jin-fa4, XIAO Qing-hui1,3, CAI Zhi-yong5(1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. Key Laboratory of Lithospheric Tectonics, Deep Process and Exploration, Ministry of Education, Beijing, 100083, China;3. China University of Geosciences, Beijing 100083, China;4. China University of Geosciences, Wuhan 430074, Hubei, China;5. Guangzhou Institute of Geochemistry,Chinese Acadeng of Science Guangzhou 510640, Guangdong, China)  
Sm-Nd and K-Ar dating of layered gabbro in the Shemalagou ophiolite in the western segment of the Bangong Co-Nujiang ophiolite belt indicates a combined internal and whole-rock Sm-Nd isochron age of 191±22 Ma and K-Ar ages of 140±4.07 Ma and 152.30±3.60 Ma. According to the dating results, combined with geological data, it is suggested that the Sm-Nd age represents the age of ocean basin opening, i.e. Early Jurassic, while the latter is the time of alteration influenced by the subduction of oceanic crust. Based on the available data in the central and eastern segments of the Bangong Co-Nujiang ophiolite belt, the ages of opening, subduction and closing of the ocean basin are discussed. The authors think that the Bangong Co-Nujiang ocean basin probably opened from east to west simultaneously in the Early Jurassic, began to be subducted southward in the Middle Jurassic and finally closed at the end of the Early Cretaceous.
【Fund】: 国家自然科学重点基金(NSFC40234048);; 国土资源部国际合作与科技司专项计划(200010103);; 中国地质调查局国土资源地质大调查项目(200113900018);; 中国地质大学“岩石圈构造、深部过程及探测技术”教育部重点实验室开放课题(2003009、2003010)联合资助。
【CateGory Index】: P597
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