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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2014-01
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LA-ICP-MS U-Pb dating of zircons and geological implication for Cenozoic volcanic rocks in Rongma area,Qiangtang terrane,North Tibet,China

RAN Hao;WANGGen-hou;LIANGXiao;ZHENGYi-long;WANGLiang;School of Earth Sciences and Resources,China University of Geosciences;Gold Geology Istitute of Chinese Armed Police Force;  
Tectonic evolution of Qiangtang terrane is studied by LA-ICP-MS U-Pb geochronology of zircons from the Cenozoic volcanic rocks in the Rongma area,Qiangtang terrane,northern Tibet.The result suggests that the ages of zircons range from Late Archean to Cenozoic(2651~24 Ma B.P.)with evident stage characteristics and fall into twelve groups:2651~1381Ma,1182~1147Ma,921~911Ma,832~741Ma,659Ma,562~535Ma,423~414Ma,320~291Ma,243~200Ma,156~140Ma,127~117Ma and 24Ma.These age groups record the tectonic thermal events of supercontinent,Pan-African Movement and Caledonian Movement.The development and evolution of the PaleoTethyan Ocean and Meso-Tethyan Ocean and the Cenozoic magmatism in the Qiangtang terrane are also recorded.They imply that there is the record of the Precambrian age.This is not the sufficient condition but the necessary condition for the existence of crystalline basement in Qiangtang terrane.There are the records of Pan-African Movement which indicate that the Qiangtang terrane,Lhasa terrane and Tethyan Himalaya are derived from Gondwana.
【Fund】: 中国地质调查局项目(1212011221115;1212011221081)
【CateGory Index】: P597.3;P588.14
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