Volume 26 Issue 2
Apr.  2020
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HAN Jian'en, LUO Peng, YU Jia, et al., 2020. Pan-lake during the late Pleistocene in the source area of the Yellow River and its significance. Journal of Geomechanics, 26 (2): 232-243. DOI: 10.12090/j.issn.1006-6616.2020.26.02.022
Citation: HAN Jian'en, LUO Peng, YU Jia, et al., 2020. Pan-lake during the late Pleistocene in the source area of the Yellow River and its significance. Journal of Geomechanics, 26 (2): 232-243. DOI: 10.12090/j.issn.1006-6616.2020.26.02.022

Pan-lake during the late Pleistocene in the source area of the Yellow River and its significance

doi: 10.12090/j.issn.1006-6616.2020.26.02.022
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  • Received: 2020-01-21
  • Revised: 2020-03-10
  • Published: 2020-04-01
  • According to the sedimentary characteristics and the results of ESR dating of the lacustrine strata profile in Maduo County, Qinghai Province, the pan-lake event had occurred in the source area of the Yellow River during the late Pleistocene period at about 130 kaB.P.. During the pan-lake period, the four lakes in Maduo County connected with each other, and formed one huge lake whose area was 4.1 times bigger than the total area of the present four lakes. The pan-lake event in the Maduo area coincided with the transition of deep sea oxygen isotope from MIS 6 to MIS 5, which shows that the climate change on the Qinghai-Tibet Plateau is closely related to the global climate change. As the lacustrine strata in the source area of the Yellow River were more sensitive to the global climate change, it recorded the climate change earlier than other areas did. The analysis of the grain size, carbonate and magnetic susceptibility of the sediments in the Maduo lacustrine strata profile shows 9 stages of the lacustrine sediments during the period of 132±10~128±12 ka, indicating a fluctuating and rising process of climate change on the Qinghai-Tibet Plateau in transition from MIS 6 to MIS 5. A large area of lacustrine sedimentation in the source area of the Yellow River ended at about 130 kaB.P. This may be the result of the regional tectonic activities of Gonghe Movement which cut through the Duoshixia gorge in the lower reaches, causing a suddenly leak out of the lake water.

     

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