Volume 46 Issue 9
Oct.  2021
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Article Navigation >  Earth Science  > 2021  >  46(9): 3245-3257
Sun Liqun, Zhang Xin, Liang Xing, Chang Zhikai, Fu Pengyu, Zhang jie, 2021. Identification and Characteristics of the Sedimentary Environment since the Quaternary in Zi River Delta, Dongting Basin. Earth Science, 46(9): 3245-3257. doi: 10.3799/dqkx.2020.357
Citation: Sun Liqun, Zhang Xin, Liang Xing, Chang Zhikai, Fu Pengyu, Zhang jie, 2021. Identification and Characteristics of the Sedimentary Environment since the Quaternary in Zi River Delta, Dongting Basin. Earth Science, 46(9): 3245-3257. doi: 10.3799/dqkx.2020.357
shu

Identification and Characteristics of the Sedimentary Environment since the Quaternary in Zi River Delta, Dongting Basin

doi: 10.3799/dqkx.2020.357

  • School of Environmental Studies, China University of Geosciences, Wuhan 430078, China

  • Received Date: 2020-10-10
    Available Online: 2021-10-14
  • Publish Date: 2021-10-14
    Abstract
  • The study of sedimentary facies and characteristics contributes to a more comprehensive understanding of river and lake environmental evolution, but there are no description of such studies in the Zi River delta, Dongting basin. Based on the Quaternary sedimentary samples of typical borehole (BMS01 and BMS02), and combined with the petrology, chronology and sedimentology study, this study uses particle size frequency distribution curves for the discriminant analysis of sedimentary facies of Quaternary deposits in the studied area. Grain size parameters of the calculation results and the Fisher discriminant model were used for verification. The results show that the Fisher model is suitable for the identification of fluvial facies, lacustrine facies and unstable facies in plain area. In the application of the discriminant function in the study area, the overall recognition accuracy rate of the discriminant function was 94.9%, and the misjudgment rate was 5.1%, which was higher than the general standard of 75% accuracy. Based on the comprehensive identification results and geological research data, this paper expounds the regional polycyclic sedimentary characteristics and evolution process since the Quaternary by using C-M diagram and particle size scatter diagram, and explains the formation mechanism of the strata. The research results could provide basic data for the classification and correlation of Quaternary strata, the evaluation of groundwater resources and the study of natural and inferior groundwater.

     

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