Volume 24 Issue 4
Aug.  2018
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Article Navigation >  Journal of Geomechanics  > 2018  >  24(4): 515-521
ZHAN Tao, ZENG Fangming, XIE Yuanyun, et al., 2018. GRAIN SIZE CHARACTERISTICS OF TIANHENGSHAN CORE AND THEIR INDICATIONS FOR STRATIGRAPHIC DIVISION IN THE EASTERN PART OF THE NORTHEAST PLAIN OF CHINA. Journal of Geomechanics, 24 (4): 515-521. DOI: 10.12090/j.issn.1006-6616.2018.24.04.054
Citation: ZHAN Tao, ZENG Fangming, XIE Yuanyun, et al., 2018. GRAIN SIZE CHARACTERISTICS OF TIANHENGSHAN CORE AND THEIR INDICATIONS FOR STRATIGRAPHIC DIVISION IN THE EASTERN PART OF THE NORTHEAST PLAIN OF CHINA. Journal of Geomechanics, 24 (4): 515-521. DOI: 10.12090/j.issn.1006-6616.2018.24.04.054
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GRAIN SIZE CHARACTERISTICS OF TIANHENGSHAN CORE AND THEIR INDICATIONS FOR STRATIGRAPHIC DIVISION IN THE EASTERN PART OF THE NORTHEAST PLAIN OF CHINA

doi: 10.12090/j.issn.1006-6616.2018.24.04.054
  • 1.

    The Second Hydrogeology and Engineering Geology Prospecting Institute of Heilongjiang Province, Harbin 150030, Heilongjiang, China

  • 2.

    State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

  • 3.

    Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, Qinghai, China

  • 4.

    College of Geographic Science, Harbin Normal University, Harbin 150025, Heilongjiang, China

  • 5.

    Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China

  • 6.

    State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

  • 7.

    Geography Department, Harbin institute, Harbin 150086, Heilongjiang, China

  • 8.

    Heilongjiang Bureau of Geology & Mineral Resources, Harbin 150036, Heilongjiang, China

  • 9.

    School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, Anhui, China

More Information
  • Received: 2017-06-26
  • Revised: 2018-02-23
  • Published: 2018-08-01
    Abstract
  • Huangshan Profile in the eastern part of the Northeast Plain is a typical Quaternary profile in Northeast China; however, there are different views on the stratigraphic division and stratigraphic origin of this section. A detailed study on its grain size characteristics is expected to provide further insight into the stratigraphic division and stratigraphic origin of the profile. In this paper, high resolution grain size characteristics of the sediments in Tianhengshan (THS) Core were studied and compared with those in typical loess profiles on the Chinese Loess Plateau. The results show that the mean grain size, median grain size and percentage fraction of grain size of Harbin Formation fluctuated widely, with coarser grains in the loess layer and finer ones in the paleosol layer, similar to those in the loess-paleosol sequence on the Chinese Loess Plateau. However, grain size characteristics in Huangshan Formation show small fluctuations, thus indicating relatively stable sedimentary dynamics. The characteristics of grain size, including frequency distribution, C-M diagram and other grain size parameters (mean grain size, standard deviation, skewness and kurtosis) in sediments between Harbin Formation and Huangshan Formation are obviously different, indicating that the sedimentary dynamics of the two groups are different. Based on the above characteristics of grain size, combining sedimentary facies and previous methods of classification, the middle-to late-Pleistocene strata of the THS Core from top to bottom is divided into Harbin Formation and Huangshan Formation, which are determined as aeolian accumulation and fluvial/lacustrine sediment, respectively.

     

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