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2018 Vol. 24, No. 2
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Maotang CAI, Peisheng YE, Xingchen YANG, Xujiao ZHANG, Chenglu LI, Wei ZHOU, Jing LU, Tao WANG. EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka[J]. Journal of Geomechanics, 2018, 24(2): 253-262. doi: 10.12090/j.issn.1006-6616.2018.24.02.027
Citation: Maotang CAI, Peisheng YE, Xingchen YANG, Xujiao ZHANG, Chenglu LI, Wei ZHOU, Jing LU, Tao WANG. EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka[J]. Journal of Geomechanics, 2018, 24(2): 253-262. doi: 10.12090/j.issn.1006-6616.2018.24.02.027
shu

EVOLUTION OF SEDIMENTARY ENVIRONMENT IN THE NORTH HETAO BASIN SINCE 344 Ka

  • 1.

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

  • 2.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

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Received Date:  10 September 2017
Revised Date:  08 January 2018
    Abstract
  • Through analysis of sedimentary facies and grain size characteristics from 377 m drilling cores in the north Hetao Basin, combined with different dating methods, the evolution of sedimentary environment in the north Hetao Basin since late Middle Pleistocene is revealed. According to the characteristics of grain size parameters, sedimentary environment can be divided into 6 stages:lakeshore (344~326 ka)-semi-deep lake (326~165 ka)-lakeshore delta (165~130 ka) -shallow lake (130~100 ka)-lakeshore-fluvial (100~10 ka)-washland (10 ka~now). Comprehensive research shows that a unified paleo-megalake has been existed in the Hetao Basin from middle Pleistocene to late Pleistocene. After late Pleistocene, the paleo-megalake disintegrated and disappeared.
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