Advanced Search
    DENG Cheng-wen, ZHANG Xia, LIN Chun-ming, XU Zhen-yu, YU Jin. Grain size analysis and environmental evolution indicated by the ZK01 borehole samples in the Changjiang delta since the latest glacial maximum[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(3): 37-46.
    Citation: DENG Cheng-wen, ZHANG Xia, LIN Chun-ming, XU Zhen-yu, YU Jin. Grain size analysis and environmental evolution indicated by the ZK01 borehole samples in the Changjiang delta since the latest glacial maximum[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(3): 37-46.

    Grain size analysis and environmental evolution indicated by the ZK01 borehole samples in the Changjiang delta since the latest glacial maximum

    More Information
    • Received Date: July 25, 2015
    • Revised Date: October 06, 2015
    • Published Date: September 29, 2016
    • The present paper gives a detailed description of grain size analysis on the basis of grain size parameters, C-M patterns, grain size probability accumulation curves and frequency distribution, and the environmental evolution according to lithology, sedimentary structures and foraminifera distribution in the Changjiang delta since the latest glacial maximum. The sediments herein can be divided into five segments from bottom to top. The riverbed deposits consist of sand and gravelly sand, and display the two-part grain size probability accumulation curves dominated by saltation populations. The floodplain deposits are made up of the interbeds of sand and clay, and display the two-part grain size probability accumulation curves represented by the suspension-dominated populations, and the bimodal or multimodal frequency distribution curves. The estuarine deposits display sharp changes of grain size parameters and C-M patterns, two-part grain size probability accumulation curves and unimodal or bimodal frequency distribution curves. The neritic deposits comprise muddy clay, and display one-part grain size probability accumulation curves represented by suspension populations. The delta deposits are significantly made up of fine sand and silt, and display the two-part grain size probability accumulation curves represented by saltation populations. The study area once underwent the evolution of river bed, floodsplain, estuary, shallow sea and delta sedimentary environments during the latest glacial maximum.
    • Related Articles

      [1]LIU Xuelong, LI Wenchang, ZHANG Shitao, LONG Qihe, MENG Guangzhi, ZHANG Hong, ZHOU Jiehu, CHENG Jialong, ZHU Jun, LU Bode, DAO Junshan, LIU Yi, CHEN Xianchao. The Late Cretaceous magmatism and Sn-Ag-Pb-Zn-W polymetallic mineralization in Bozhushan ore concentration area, southeast Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2024, 44(2): 437-453. DOI: 10.19826/j.cnki.1009-3850.2024.04006
      [2]LU Chang, XIA Guoqing, CHEN Yun, WU Jinxuan, BAO Wancheng, FAN Qiushuang, SHI Zhu, HAO Xiawei. Late Eocene-Early Oligocene clay mineral characteristics and paleoclimate significance in Lunpola Basin, Tibet[J]. Sedimentary Geology and Tethyan Geology, 2023, 43(3): 565-579. DOI: 10.19826/j.cnki.1009-3850.2023.02021
      [3]NIE fei, LIU Shusheng, YANG Yongfei, PENG Zhimin, GUO Linnan. Zircon U-Pb dating and its geological implications for the diorites from the Phu Lon skarn-type copper-gold deposit in Thailand[J]. Sedimentary Geology and Tethyan Geology, 2019, 39(4): 71-78.
      [4]REN Hong-yu, FU Heng, Ji Jia, Guan Yue-shan, ZHU Da. Correlation of Cretaceous-Palaeogene sedimentary evolution in southwestern Tarim Basin and adjacent central Asia basins[J]. Sedimentary Geology and Tethyan Geology, 2017, 37(3): 103-112.
      [5]MA Guo-tao, LIU Hong, HUANG Han-xiao, CHEN Min-hua, LAN Shuang-shuang, LU Meng-hong, XIE Hui. Metallogenic conditions and prospecting potential of orogenic gold deposits in the central western part of Bangong Lake-Nujiang metallogenic zone[J]. Sedimentary Geology and Tethyan Geology, 2017, 37(3): 89-95.
      [6]WANG Jiang-li, LIN Fang-cheng, ZHU Hua-ping, WANG Hong, SHI Mei-feng. SHRIMP zircon U-Pb dating of the ore-forming monzogranite from the Phalek iron deposit, Vientiane, Laos and its geological implications[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(3): 87-93.
      [7]SHI Mei-feng, LIN Fang-cheng, LIU Chao-ji, LI Xing-zhen, WANG Hong. Classification and metallogenesis of metallogenic belts in Southeast Asia and the neighbouring southwestern part of China[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(2): 103-112.
      [8]ZHANG Bin, ZHANG Lin-kui, CHEN Min-hua, LIU Shu-sheng, JIAO Yan-jie. Geology and significance of the Bajiaoqing lead-zinc deposit in Xichou, southeastern Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(2): 94-101.
      [9]FU Heng, FANG Xiao-lu, JIANG Shao-zhen. Cratering events in the Japan Sea and tectonic evolution of East Asia during the Cenozoic[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(1): 93-97.
      [10]Wang Chengshu. Active subduction and collision in Southeast Asia[J]. Sedimentary Geology and Tethyan Geology, 2002, 22(1): 92-112.

    Catalog

      Article views (118) PDF downloads (72) Cited by()

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return