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《Geology in China》 2007-06
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Chronology of Pliocene-early Pleistocene lacustrine strata in the Zanda basin, Ngari area, Tibet

ZHU Da-gang1, MENG Xian-gang1, SHAO Zhao-gang1, YANG Chao-bin2, Wang Jin1, HAN Jian-en1, YU Jia2, MENG Qing-wei1, Lū Rong-ping1 (1. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 2. Department of Land and Resources of the Tibet Autonomous Region, Lhasa 850000, Tibet, China)  
Neogene Pliocene-Quaternary early Pleistocene strata have been determined through analyses of paleomagnetic and ESR samples from a section of fluvio-lacustrine strata in the Zanda basin, Ngari, Tibet. The analytic results show that: the paleomagnetic ages obtained in ascending order from the section are 5.41-1.60 Ma, while the ESR ages are 5.40-1.36 Ma. The two analytic results roughly coincide. According to the results of the paleomagnetic and ESR datings, the time series of the fluvio-lacustrine strata is as follows: the Pliocene Tolin Formation (N12t) formed at 5.41-4.20 Ma, the Pliocene Guge Formation (N22g) formed at 4.20-2.57 Ma and the Quaternary early Pleistocene Qangzê Formation (Qp1-1x) formed at 2.57-1.36 Ma. This study provides an important basis for the establishment of the time scale of the Neogene Pliocene-Quaternary early Pleistocene strata on the Qinghai-Tibet Plateau and division and correlation of the Neogene Pliocene-Quaternary early Pleistocene fluvio-lacustrine strata.
【Fund】: 国家自然科学基金项目(40572134);; 中国地质调查局地质大调查项目(1212010511902、1212010611703、1212010610108、1212010711705)
【CateGory Index】: P539
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9 Kuang Mingsheng 1 , Li Jijun 2 , Zhao Yu 3 , Chen Xunqian 3 , Zhang Yaping 3 and Guo Tianxiong 3 (1 Department of Geography, Southwest China Normal University, Chongqing 630715; 2 Department of Geography, Lanzhou University,;A Study on the Quaternary Glacial Relics in the Gongwang Mountains in the Northeast Part of Yunnan Province[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;1997-04
10 WANG Weiliang ZHANG Jinjiang 1) ZHANG Bo (School of Earth and Space Sciences, Peking University, Beijing, 100871;Structural and Sedimentary Features in Zanda Basin of Tibet[J];Acta Scicentiarum Naturalum Universitis Pekinesis;2004-06
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