WANG Xian-yan, LU Hua-yu, YI Shuang-wen, DENG Cheng-long. EXTENSION OF THE TYPICAL AEOLIAN SEQUENCES AT LUOCHUAN, CENTRAL CHINESE LOESS PLATEAU[J]. Marine Geology & Quaternary Geology, 2006, 26(1): 89-92.
Citation: WANG Xian-yan, LU Hua-yu, YI Shuang-wen, DENG Cheng-long. EXTENSION OF THE TYPICAL AEOLIAN SEQUENCES AT LUOCHUAN, CENTRAL CHINESE LOESS PLATEAU[J]. Marine Geology & Quaternary Geology, 2006, 26(1): 89-92.
shu

EXTENSION OF THE TYPICAL AEOLIAN SEQUENCES AT LUOCHUAN, CENTRAL CHINESE LOESS PLATEAU

  • 1 SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China;

  • 2 Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;

  • 3 Department of Geography, Nanjing University, Nanjing 210093, China;

  • 4 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

More Information
  • Received Date: May 30, 2005
  • Revised Date: October 08, 2005
    Graphical Abstract
    • Abstract
  • In this work,the ‘Red Clay’ deposit underlying the typical loess-paleosol sequence at Luochuan,central Chinese Loess Plateau,is studied on magnetostratigraphy,grain size distribution and magnetic susceptibility.It shows that aeolian deposit of the late Cenozoic at Luochuan,the National Loess Park,started at least since 3.2 Ma before present.Proxy index of paleoclimate of this aeolian sequence such as grain size distribution and magnetic susceptibility indicates that the paleoclimate was relatively warmer and less varied during the late Pliocene than that of the loess deposit during the Quaternary period and there was a significant climate shifting that took place around 2.6 MaBP,the boundary of the Pliocene and Pleistocene in North China.
    • FullText(HTML)
    • References (18)
  • [1]
    Heller F, LIU Tung-sheng. Magnetostratigraphical dating of loess deposits in China[J]. Nature, 1982, 300:413-433.
    [2]
    刘东生.黄土与环境[M]. 北京:科学出版社, 1985.[LIU Tung-sheng. Loess and the Environment[M].Beijing:Science Press,1985.]
    [3]
    王永炎. 中国黄土研究的新进展[M].西安:陕西人民出版社,1985.[WANG Yong-yan. The New Development of Loess Studies in China[M].Xi'an:Shannxi People Press, 1985.]
    [4]
    Kukla G, AN Zhi-sheng. Loess stratigraphy in central China[J]. Palaeogeography, Palaeolimatology, Palaeoecology,1989, 72:203-225.
    [5]
    安芷生,Kukla G, 刘东生. 洛川黄土地层学[J]. 第四纪研究,1989,9(2):155-168.

    [AN Zhi-sheng, Kukla G,LIU Tung-sheng. Loess stratigraphy in Luochuan, central China[J]. Quaternary Sciences,1989,9(2):155-168.]
    [6]
    AN Zhi-sheng, Kukla G, Porter S C, et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130000 years[J].Quaternary Research, 1991, 36:29-36.
    [7]
    LU Hua-yu, LIU Xiao-dong, ZHANG Fu-qing, et al. Astronomical calibration of loess paleosol deposits at Luochuan, central Chinese Loess Plateau[J].Paleogeography, Palaeoclimatology, Palaeoecology, 1999a, 154(3):237-246.
    [8]
    LU Hua-yu, Huissteden K V, AN Zhi-sheng, et al. East Asia winter monsoon variation on a millennial time scale before the last glacial-interglacial cycle[J]. Journal of Quaternary Science, 1999b, 14(2):101-110.
    [9]
    DING Zhong-li, Rutter N W, SUN Ji-min,et al. Rearrangement of atmospheric circulation at about 2.6 Ma over northern China:evidence from grain size records of loess-palaeosol and red clay sequences[J]. Quaternary Science Reviews, 2000,19(6):547-558.
    [10]
    Han J, Fyfe W S, Gu Z.Assessment of the palaeoclimate during 3.0~2.6 Ma registered by transition of Red Clay to loess-palaeosol sequence in central North China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 185:355-368.
    [11]
    LU Hua-yu, AN Zhi-sheng. Pretreated methods on loess-palaeosol samples granulometry[J]. Chinese Science Bulletin, 1998, 43(3):237-240.
    [12]
    GUO Zheng-tang, PENG Shu-zhen, HAO Qin-zhen, et al. Origin of the Miocene-Pliocene red-earth formation at Xifeng in northern China and implications for paleoenvironments[J]. Paleogeography, Palaeoclimatology, Palaeoecology, 2001, 170:11-26.
    [13]
    汶玲娟,鹿化煜,强小科. 新近纪黄土高原红黏土粒度和沉积速率的空间变化及其揭示的古大气粉尘传输动力[J]. 中国科学D辑, 2004, 34(8):739-747.

    [WEN Ling-juan, LU Hua-yu, QIANG Xiao-ke. Changes in grain-size and sedimentation rate of the Neogene Red Clay deposits along the Chinese Loess Plateau and implications for the palaeowind system[J]. Science in China(Series D), 2004, 34(8):739-747.]
    [14]
    MIAO Xiao-dong, SUN You-bin, LU Hua-yu,et al.Spatial pattern of grain size in the Late Pliocene ‘Red Clay’ deposits (North China) indicates transport by low-level northerly winds[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004, 206:149-155.
    [15]
    DING Zhong-li, Yu Z, Rutter N W, et al. Towards an orbital time scale for Chinese loess deposits[J].Quaternary Science Reviews, 1994, 13(1):39-70.
    [16]
    鹿化煜,安芷生. 洛川黄土粒度组成的古气候意义[J].科学通报,1997,42(1):67-69.

    [LU Hua-yu, AN Zhi-sheng. Paleoclimatic significance of loess granularity compositions in Loess Plateau[J]. Science in China(Series D),1998,28(3):278-283.]
    [17]
    GUO Zheng-tang, PENG Shu-zhen, Biscaye P E, et al. Late Miocene-Pliocene development of Asian aridification as recorded in the Red-Earth Formation in northern China[J]. Global and Planetary Change, 2004, 41:135-145.
    [18]
    Cande S C, Kent D V. Revised calibration of the geomagnetic polarity time scale for the late Cretaceous and Cenozoic[J]. Journal of Geophysical Research, 1995, 100:6093-6095.
    • Related Articles

  • Related Articles

    [1]LI Canping, BAO Binghuang, CHANG Liang, ZHANG Hairong, CHEN Fengying, WANG Rui, HUANG Yuhui. Simulation of hydrate and free gas reservoirs based on random medium theory[J]. Marine Geology & Quaternary Geology, 2025, 45(1): 199-209. DOI: 10.16562/j.cnki.0256-1492.2023112701
    [2]MAO Peixiao, WU Nengyou, WAN Yizhao, CHEN Qiang, HU Gaowei. Effects of perforation degree and deployment position of multilateral horizontal wells on gas production from inclined clay hydrate reservoirs[J]. Marine Geology & Quaternary Geology, 2022, 42(6): 207-217. DOI: 10.16562/j.cnki.0256-1492.2022011501
    [3]JIANG Xue, XIONG Zhiwu. Semi-quantitative study on reservoir configuration in grey theory—A case study of H3 sand unit of Huagang Formation in A Structure, Xihu Sag[J]. Marine Geology & Quaternary Geology, 2022, 42(6): 162-172. DOI: 10.16562/j.cnki.0256-1492.2022022301
    [4]YUAN Yong, CHEN Jianwen, LIANG Jie, ZHANG Yinguo, XUE Lu, WU Shuyu, LAN Tianyu, WU Piao. Characteristics and hydrocarbon prospects of the Permian sandstone reservoirs of the Laoshan Uplift, South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2021, 41(5): 181-193. DOI: 10.16562/j.cnki.0256-1492.2021020201
    [5]LUO Jian, HU Wengliang, HE Yuchun, LIU Chunfeng, WANG Meng. Logging evaluation for low permeability reservoirs under different mud systems in East China Sea[J]. Marine Geology & Quaternary Geology, 2019, 39(6): 216-227. DOI: 10.16562/j.cnki.0256-1492.2019070403
    [6]MIAO Qing, ZHANG Wu, ZHAO Xingbin, XIAO Xiaoguang, LI Junjie. The development model for high quality magmatic basement reservoir in a depression of East China Sea[J]. Marine Geology & Quaternary Geology, 2019, 39(6): 93-101. DOI: 10.16562/j.cnki.0256-1492.2019070502
    [7]WU Qilin, HUANG SiJing, DAN Zhiwei, XIAO Wei, ZENG Yi, ZHOU Xiaokang, HOU Zhiping. PREDICTION OF CARBONATE RESERVOIRS IN BLOCK A OF HUIZHOU AREA IN PEARL RIVER MOUTH BASIN[J]. Marine Geology & Quaternary Geology, 2015, 35(2): 149-155. DOI: 10.3724/SP.J.1140.2015.02149
    [8]ZHANG Xiuli, PEI Jianxin, WANG Qi. PRELIMINARY STUDY OF PARAMETERS DESIGN FOR EXPLORATION OF HIGH RESISTIVITY RESERVOIR USING MARINE CSEM METHOD[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 181-188. DOI: 10.3724/SP.J.1140.2014.04181
    [9]ZENG Xiaoming, YU Xinghe, LIANG Jinqiang, KUANG Zenggui, WANG Jianzhong. GEOLOGICAL MODEL AND PREDICTION FOR FAVORABLE AREAS OF NATURAL GAS HYDRATE IN SHENHU AREA[J]. Marine Geology & Quaternary Geology, 2014, 34(4): 117-126. DOI: 10.3724/SP.J.1140.2014.04117
    [10]LI Junliang, ZUO Qianmei, XIE Xinong, ZHANG Cheng, ZHONG Zehong. NEOGENE DEPOSITIONAL FEATURES AND FAVORABLE RESERVOIR-CAP COMBINATIONS IN THE DEEPWATER OF QIONGDONGNAN BASIN, NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(6): 109-116. DOI: 10.3724/SP.J.1140.2011.06109

Catalog

    Get Citation
    PDF
    XML
    Article views PDF downloads Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return