• The Core Journal of China
  • Included in Chinese Scientific and Technical Papers and Citations Database
  • Included in Chinese Science Citation Database (CSCD)
  • Included in Chemical Abstracts (CA)
  • Included in Scopus
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]LIANG Lei, XU Guoqiang, HUANG Wuxuan, LIANG Dingyong, LI Sunxiong, HAO Qiang, HUANG Rong. Environmental evolution and its driving mechanisms of southeastern Beibu Gulf since the Last glacial period[J]. Sedimentary Geology and Tethyan Geology, 2023, 43(4): 702-711. DOI: 10.19826/j.cnki.1009-3850.2021.09001
    [2]YU Rui-xue, LI Chang-you, LI Wen-bao, ZHEN Zhi-lei, ZHAO Sheng-nan, ZHANG Shuai. Sedimentary environmental and stratigraphic analysis of the sensitive grain size components from the Dalai Nur Lake deposits, Inner Mongolia[J]. Sedimentary Geology and Tethyan Geology, 2016, 36(3): 77-82.
    [3]LI Ming-long, ZHENG De-shun, GONG Wen-lei, ZHOU Lu, CHENG Yong. Grain size analysis for the sandstones from the Middle Jurassic Ma'ao Formation in the Jiyuan Basin, Henan[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(2): 25-31.
    [4]YING Li-chao, LIANG Bin, WANG Quan-wei, ZHU Bing, HAO Xue-feng, WANG Xin, LIU Liang, FU Xiao-fang. Grain size analysis and origin of the Chengdu clay from the Chengdu Plain, Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(1): 72-77.
    [5]ZHENG Wei, QI Yong-an, XING Zhi-feng, YUAN Yu-yang. Microbially induced sedimentary structures and sedimentary environments of the Ruyang Group in Lushan,western Henan[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(1): 24-31.
    [6]CAO Gao-she, YANG Qi-hao, LIN Yu-xiang, XING Nana, ZU Xin-xu, XU Guang-ming. Grain size analysis of the Upper Triassic deposits in the Liushan Basin,Henan[J]. Sedimentary Geology and Tethyan Geology, 2009, 29(3): 9-14.
    [7]NI Hua-yong, LIU Xi-lin. Grain-size distribution and fractal structures of solid grains in debris-flow deposits[J]. Sedimentary Geology and Tethyan Geology, 2008, 28(3): 35-40.
    [8]LIU Yan-lin, YUE Le-ping, Palati. Grain-size distribution and palaeoenvironmental significance for the Neogene red clay in the middle reaches of the Huanghe River: An example from the Laogaochuan section in Fugu, Shaanxi[J]. Sedimentary Geology and Tethyan Geology, 2004, 24(1): 78-83.
    [9]Zhang Tingshan, Yu Jianhua, Bian Lizeng, S. Kershaw, Chen Xiaohui, Lan Guangzhi, Wan Yun. Strontium,carbon and oxygen isotopic compositions and their geological significance:the Silurian strata on the northern and southern margins of the Sichuan Basin[J]. Sedimentary Geology and Tethyan Geology, 1998, 18(3): 41-49.
    [10]Yan Guoshun, Zhang Enhui, Wang Deyou. EVOLUTION OF NORTH CHINA-TYPE EARLY CAMBRIAN SEDIMENTARY ENVIRONMENTS AND TRACE FOSSIL ASSEMBLAGES IN HENAN PROVINCE[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(3): 18-32.

Catalog

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

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return