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2021 Vol. 27, No. 6
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KOU Linlin, LI Zhenhong, DONG Xiaopeng, CUI Jiawei, LI Hailong. 2021. The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Xizang Plateau, and its geological significance. Journal of Geomechanics, 27(6): 1051-1064. doi: 10.12090/j.issn.1006-6616.2021.27.06.085
Citation: KOU Linlin, LI Zhenhong, DONG Xiaopeng, CUI Jiawei, LI Hailong. 2021. The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Xizang Plateau, and its geological significance. Journal of Geomechanics, 27(6): 1051-1064. doi: 10.12090/j.issn.1006-6616.2021.27.06.085
shu

The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Xizang Plateau, and its geological significance

  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    Chinese Academy of Geological Sciences, Beijing 100037, China

  • 3.

    Key Laboratory of Paleomagnetism and Tectonic Reconstruction of Ministry of Natural Resources, Beijing 100081, China

    • Fund Project: This research is financially supported by the National Natural Science Foundation of China (Grant No. 41972119) and the Geological Survey Project of China Geological Survey (Grant No. DD20190018)
More Information
Received Date:  25 April 2021
Revised Date:  11 August 2021
Publish Date:  28 December 2021
    Abstract

  • The precise age of the strata at the northeastern margin of the Xizang Plateau in the Paleogene-Neogene, and the initial time when the uplift of the Plateau affected its northeastern margin, have always been two main bone contentions among geologists. The Guanyindian section at the northeastern margin of the Xizang Plateau is our research subject. We gain new insights to the two mentioned issues by using detrital zircon U-Pb dating in combination with the previous results concerning regional paleontological fossil identification and paleomagnetic dating. The dating results show, among the samples from the upper Paleogene Qingshuiying formation at the northeastern margin of the Xizang Plateau, the youngest peak is 17.8 Ma. Two conclusions are drawn from the research results. Firstly, the deposition age of the Qingshui formation is from the late Oligecene to early Miocene, showing the characteristic of diachronism. Secondly, the northeastward extension and pushing of the uplift of the Xizang Plateau has begun affecting the west of the Haiyuan-Liupanshan fault zone since the early Miocene with a coupling relationship among tectonics, sedimentation and climate in the area. The research findings provide a new time scale for determining the initial time when the northeastward pushing of the Xizang Plateau began to affect its northeastern margin.

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