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Zhou YANG, Shubing WANG, Fuchu JIANG, Xisheng WANG, Jianli FU. DISCUSSION ON MANGSHAN LOESS STRATIGRAPHIC DIVISON IN CHINA CENTRAL PLAINS[J]. Journal of Geomechanics, 2018, 24(2): 274-282. doi: 10.12090/j.issn.1006-6616.2018.24.02.029
Citation: Zhou YANG, Shubing WANG, Fuchu JIANG, Xisheng WANG, Jianli FU. DISCUSSION ON MANGSHAN LOESS STRATIGRAPHIC DIVISON IN CHINA CENTRAL PLAINS[J]. Journal of Geomechanics, 2018, 24(2): 274-282. doi: 10.12090/j.issn.1006-6616.2018.24.02.029
shu

DISCUSSION ON MANGSHAN LOESS STRATIGRAPHIC DIVISON IN CHINA CENTRAL PLAINS

  • 1.

    Henan Xinyang Hydrology and Water Resources Survey Bureau, Xinyang 464000, Henan, China

  • 2.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

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Received Date:  25 October 2017
Revised Date:  25 December 2017
    Abstract
  • Stratigraphic age and stratigraphic division are basic and pilot work. As the research moves along, stratigraphic division will be re-recognized. The age and division of the loess stratigraphy mainly depend on OSL, 14C, paleomagnetism and magnetic susceptibility. Mangshan is famous for the extremely thick Manlan loess, while there exists different understandings about the stratigraphic division. Early research about Zhaoxiayu section revealed that the thickness of L1 is 98m, with the weakly developed palaeosol L1SS1, and the oldest stratum exposed at the bottom of the section is the palaeosol S10. Later, the early L1 layer was divided into L1, S1 and L2 layers, and the oldest layer at the bottom of the section is the palaeosol S11 layer. Based on detailed paleomagnetic study of B/M boundary, combined with previous dating results, it is believed that the early division of L1 and the confirmation of the oldest stratum are correct, but the position of B/M boundary is mislocated. The late-stage studies are right in the position of B/M boundary but wrong in the confirmation of the oldest stratum, and also it's not appropriate to divide the palaeosol layer L1SS1 of the Malan Loess into S1. The stratigraphic correlation shows that the Mangshan loess include S0-S10 loess-palaeosol sequence, and the B/M boundary is located at the bottom of the loess L8.
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  • 蒋复初, 吴锡浩, 肖华国, 等.郑州邙山桃花峪高分辨率晚更新世黄土地层[J].地质力学学报, 1997, 3(2):11~17.

    Google Scholar

    JIANG Fuchu, WU Xihao, XIAO Huaguo, et al. The high-resolution late Pleistocene loess stratigraphy in Taohuayu, Mangshan, Zhengzhou[J]. Journal of Geomechanics, 1997, 3(2):11~17. (in Chinese with English abstract)

    Google Scholar

    杨革联, 赵希涛, 朱日祥, 等.河南荥阳孤柏嘴黄土剖面磁性地层学初步研究[J].现代地质, 2001, 15(1):35~39.

    Google Scholar

    YANG Gelian, ZHAO Xitao, ZHU Rixiang, et al. A Preliminary study in magnetostratigraphy of Gubaizui loess section in Xingyang, Henan Province[J]. Geoscience, 2001, 15(1):35~39. (in Chinese with English abstract)

    Google Scholar

    蒋复初, 吴锡浩, 孙东怀, 等.中原邙山黄土地层[J].地质力学学报, 1998, 4(4):12~18.

    Google Scholar

    JIANG Fuchu, WU Xihao, SUN Donghuai, et al. On Mangshan loess stratigraphy in China central plains[J]. Journal of Geomechanics, 1998, 4(4):12~18. (in Chinese with English abstract)

    Google Scholar

    蒋复初, 吴锡浩, 肖华国, 等.中原邙山黄土及构造与气候耦合作用[J].海洋地质与第四纪地质, 1999, 19(1):45~51.

    Google Scholar

    JIANG Fuchu, WU Xihao, XIAO Huaguo, et al. Mangshan loess in China Central Plains and the coupling effect between tectonics and climate[J]. Marine Geology & Quaternary Geology, 1999, 19(1):45~51. (in Chinese with English abstract)

    Google Scholar

    蒋复初, 王书兵, 赵志中, 等.中原邙山黄土与末次间冰期以来古季风特征[J].地质论评, 2004, 50(5):554~560.

    Google Scholar

    JIANG Fuchu, WANG Shubing, ZHAO Zhizhong, et al. The Mangshan loess in Central China and Paleomonsoon characteristic since the last interglacial stage[J]. Geological Review, 2004, 50(5):554~560. (in Chinese with English abstract)

    Google Scholar

    Wu X H, Jiang F C, Xiao H G, et al. Mangshan loess on China's Central Plain and its response to tectonic movement and climate[J]. Science in China (Series D), 1999, 42(5):465~473. doi: 10.1007/BF02875240

    CrossRef Google Scholar

    Jiang F C, Wang S B, Zhao Z Z, et al. Mangshan loess in Central China and the Paleomonsoon variations since the Last Interglaciation[J]. Acta Geologica Sinica (English Edition), 2004, 78(3):813~819.

    Google Scholar

    Jiang F C, Fu J L, Wang S B, et al. Formation of the Yellow River, inferred from loess-palaeosol sequence in Mangshan and lacustrine sediments in Sanmen Gorge, China[J]. Quaternary International, 2007, 175(1):62~70. doi: 10.1016/j.quaint.2007.03.022

    CrossRef Google Scholar

    Xiao H G, Wu X H, Jiang F C, et al. The Palaeoclimate variations in the central plains since the interstade of the Last Glacial stage[J]. Acta Geologica Sinica (English Edition), 1998, 72(1):108~119.

    Google Scholar

    Prins M A, Zheng H B, Beets K, et al. Dust supply from river floodplains:the case of the lower Huang He (Yellow River) recorded in a loess-palaeosol sequence from the Mangshan Plateau[J]. Journal of Quaternary Science, 2009, 24(1):75~84.

    Google Scholar

    Peterse F, Prins M A, Beets C J, et al. Decoupled warming and monsoon precipitation in East Asia over the last deglaciation[J]. Earth and Planetary Science Letters, 2011, 301(1/2):256~264.

    Google Scholar

    Peterse F, Martínez-García A, Zhou B, et al. Molecular records of continental air temperature and monsoon precipitation variability in East Asia spanning the past 130, 000 years[J]. Quaternary Science Reviews, 2014, 83:76~82. doi: 10.1016/j.quascirev.2013.11.001

    CrossRef Google Scholar

    陈立业, 张珂, 傅建利, 等.邙山黄土L5以来的常量元素地球化学特征及其对物源的指示意义[J].第四纪研究, 2017, 37(6):1293~1308.

    Google Scholar

    CHEN Liye, ZHANG Ke, FU Jianli, et al. Major element geochemical characteristics of Mangshan Loess since L5 and its implications for provenance[J]. Quaternary Sciences, 2017, 37(6):1293~1308. (in Chinese with English abstract)

    Google Scholar

    Jin C S, Liu Q S. Revisiting the stratigraphic position of the Matuyama-Brunhes geomagnetic polarity boundary in Chinese loess[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 299(1/2):309~317.

    Google Scholar

    Zheng H B, Huang X T, Ji J L, et al. Ultra-high rates of loess sedimentation at Zhengzhou since Stage 7:Implication for the Yellow River erosion of the Sanmen Gorge[J]. Geomorphology, 2007, 85(3/4):131~142.

    Google Scholar

    季军良, 郑洪波, 刘锐, 等.邙山黄土地层再研究[J].海洋地质与第四纪地质, 2004, 24(4):101~108.

    Google Scholar

    JI Junliang, ZHENG Hongbo, LIU Rui, et al. Restudy on the stratigraphy of Mangshan loess[J]. Marine Geology & Quaternary Geology, 2004, 24(4):101~108. (in Chinese with English abstract)

    Google Scholar

    Qiu F Y, Zhou L P. A new luminescence chronology for the Mangshan loess-palaeosol sequence on the southern bank of the Yellow River in Henan, central China[J]. Quaternary Geochronology, 2015, 30:24~33. doi: 10.1016/j.quageo.2015.06.014

    CrossRef Google Scholar

    王玉振, 王书兵, 王喜生, 等.郑州邙山官庄峪黄土地层研究[J].地质力学学报, 2015, 21(3):393~398.

    Google Scholar

    WANG Yuzhen, WANG Shubing, WANG Xisheng, et al. Study on the Guanzhuangyu loess stratigraphy in Mangshan, Zhengzhou[J]. Journal of Geomechanics, 2015, 21(3):393~398. (in Chinese with English abstract)

    Google Scholar

    Jin C S, Liu Q S. Remagnetization mechanism and a new age model for L9 in Chinese loess[J]. Physics of the Earth and Planetary Interiors, 2011, 187(3/4):261~275.

    Google Scholar

    Liu Q S, Roberts A P, Rohling E J, et al. Post-depositional remanent magnetization lock-in and the location of the Matuyama-Brunhes geomagnetic reversal boundary in marine and Chinese loess sequences[J]. Earth and Planetary Science Letters, 2008, 275(1/2):102~110.

    Google Scholar

    Yang T S, Hyodo M, Yang Z Y, et al. Multiple rapid polarity swings during the Matuyama-Brunhes transition from two high-resolution loess-paleosol records[J]. Journal of Geophysical Research:Solid Earth, 2010, 115(B5):B05101, doi:10.1029/2009JB006301.

    CrossRef Google Scholar

    Wang X S, Løvlie R, Chen Y, et al. The Matuyama-Brunhes polarity reversal in four Chinese loess records:High-fidelity recording of geomagnetic field behavior or a less than reliable chronostratigraphic marker?[J]. Quaternary Science Reviews, 2014, 101:61~76. doi: 10.1016/j.quascirev.2014.07.005

    CrossRef Google Scholar

    Wang X S, Yang Z Y, Løvlie R, et al. A magnetostratigraphic reassessment of correlation between Chinese loess and marine oxygen isotope records over the last 1.1 Ma[J]. Physics of the Earth and Planetary Interiors, 2006, 159(1/2):109~117.

    Google Scholar

    Wang X S, Løvlie R, Yang Z Y, et al. Remagnetization of Quaternary eolian deposits:a case study from SE Chinese Loess Plateau[J]. Geochemistry, Geophysics, Geosystems, 2005, 6(6):Q06H18, doi:10.1029/2004GC000901.

    CrossRef Google Scholar

    王喜生, 杨振宇, REIDAR L, 等.三门峡地区黄土L9的重磁化现象及原因探析[J].第四纪研究, 2005, 25(4):453~460.

    Google Scholar

    WANG Xisheng, YANG Zhenyu, REIDAR L, et al. Remagnetization of L9 in the Sanmenxia area and preliminary analysis of remagnetization mechanisms[J]. Quaternary Sciences, 2005, 25(4):453~460. (in Chinese with English abstract)

    Google Scholar

    Wang D J, Wang Y C, Han J T, et al. Geomagnetic anomalies recorded in L9 of the Songjiadian loess section in southeastern Chinese Loess Plateau[J]. Chinese Science Bulletin, 2010, 55(6):520~529, doi:10.1007/s11434-009-0565-9.

    CrossRef Google Scholar

    Liu W M, Zhang L Y. Chemical magnetization in Chinese loess[J]. Physics of the Earth and Planetary Interiors, 2013, 218:14~18. doi: 10.1016/j.pepi.2013.02.005

    CrossRef Google Scholar

    刘维明, 张立原, 孙继敏.高分辨率洛川剖面黄土磁性地层学[J].地球物理学报, 2010, 53(4):888~894, doi:10.3969/j.issn.0001-5733.2010.04.013.

    CrossRef Google Scholar

    LIU Weiming, ZHANG Liyuan, SUN Jimin. High resolution magnetostratigraphy of the Luochuan loess-paleosol sequence in the central Chinese Loess Plateau[J]. Chinese Journal of Geophysics, 2010, 53(4):888~894, doi:10.3969/j.issn.0001-5733.2010.04.013.(in Chinese with English abstract)

    CrossRef Google Scholar

    Sun J M, Liu T S. Stratigraphic evidence for the uplift of the Tibetan Plateau between -1.1 and -0.9 myr ago[J]. Quaternary Research, 2000, 54(3):309~320. doi: 10.1006/qres.2000.2170

    CrossRef Google Scholar

    Evans M E, Heller F. Magnetism of loess/palaeosol sequences:Recent developments[J]. Earth-Science Reviews, 2001, 54(1/3):129~144.

    Google Scholar

    Rhodes E J. Optically stimulated luminescence dating of sediments over the past 200, 000 years[J]. Annual Review of Earth and Planetary Sciences, 2011, 39:461~488. doi: 10.1146/annurev-earth-040610-133425

    CrossRef Google Scholar

    康树刚, 王旭龙, 王松娜.中国黄土释光测年与应用:过去、现在与未来[J].地球环境学报, 2016, 7(5):442~467. doi: 10.7515/JEE201605002

    CrossRef Google Scholar

    KANG Shugang, WANG Xulong, WANG Songna. Luminescence dating of Chinese loess and its applications:Past, present and future[J]. Journal of Earth Environment, 2016, 7(5):442~467. (in Chinese with English abstract) doi: 10.7515/JEE201605002

    CrossRef Google Scholar

    Li B, Roberts R G, Jacobs Z, et al. Construction of a 'global standardised growth curve' (gSGC) for infrared stimulated luminescence dating of K-feldspar[J]. Quaternary Geochronology, 2015, 27:119~130. doi: 10.1016/j.quageo.2015.02.010

    CrossRef Google Scholar

    Li B, Roberts R G, Jacobs Z, et al. Potential of establishing a 'global standardised growth curve' (gSGC) for optical dating of quartz from sediments[J]. Quaternary Geochronology, 2015, 27:94~104. doi: 10.1016/j.quageo.2015.02.011

    CrossRef Google Scholar

    Li B, Li S H. Luminescence dating of Chinese loess beyond 130 ka using the non-fading signal from K-feldspar[J]. Quaternary Geochronology, 2012, 10:24~31. doi: 10.1016/j.quageo.2011.12.005

    CrossRef Google Scholar

    Li B, Jacobs Z, Roberts R G, et al. Extending the age limit of luminescence dating using the dose-dependent sensitivity of MET-pIRIR signals from K-feldspar[J]. Quaternary Geochronology, 2013, 17:55~67.

    Google Scholar

    Chen Y W, Li S H, Li B, et al. Maximum age limitation in luminescence dating of Chinese loess using the multiple-aliquot MET-pIRIR signals from K-feldspar[J]. Quaternary Geochronology, 2015, 30:207~212. doi: 10.1016/j.quageo.2015.01.002

    CrossRef Google Scholar

    Wang X L, Wintle A G, Lu Y C. Thermally transferred luminescence in fine-grained quartz from Chinese loess:basic observations[J]. Radiation Measurements, 2006, 41(6):649~658. doi: 10.1016/j.radmeas.2006.01.001

    CrossRef Google Scholar

    Wang X L, Lu Y C, Wintle A G. Recuperated OSL dating of fine-grained quartz in Chinese loess[J]. Quaternary Geochronology, 2006, 1(2):89~100.

    Google Scholar

    刘嘉麒, 陈铁梅, 聂高众, 等.渭南黄土剖面的年龄测定及十五万年来高分辨时间序列的建立[J].第四纪研究, 1994, 14(3):193~202.

    Google Scholar

    LIU Jiaqi, CHEN Tiemei, NIE Gaozhong, et al. Datings and reconstruction of the high resolution time series in the Weinan loess section of the last 150000 years[J]. Quaternary Sciences, 1994, 14(3):193~202. (in Chinese with English abstract)

    Google Scholar

    王文远, 刘嘉麒, 潘懋, 等.末次间冰期以来黄土-古土壤的热释光测年-渭南、会宁剖面的对比研究[J].海洋地质与第四纪地质, 2000, 20(3):67~72.

    Google Scholar

    WANG Wenyuan, LIU Jiaqi, PAN Mao, et al. Thermoluminescent dating of the loess sequence of the late Quaternary-the comparing study on the Weinan and Huining sections[J]. Marine Geology & Quaternary Geology, 2000, 20(3):67~72. (in Chinese with English abstract)

    Google Scholar

    Lu Y C, Wang X L, Wintle A G. A new OSL chronology for dust accumulation in the last 130, 000 yr for the Chinese Loess Plateau[J]. Quaternary Research, 2007, 67(1):152~160.

    Google Scholar

    Lai Z P. Chronology and the upper dating limit for loess samples from Luochuan section in the Chinese Loess Plateau using quartz OSL SAR protocol[J]. Journal of Asian Earth Sciences, 2010, 37(2):176~185. doi: 10.1016/j.jseaes.2009.08.003

    CrossRef Google Scholar

    Kang S G, Lu Y C, Wang X L. Closely-spaced recuperated OSL dating of the last interglacial paleosol in the southeastern margin of the Chinese Loess Plateau[J]. Quaternary Geochronology, 2011, 6(5):480~490.

    Google Scholar

    Lü T Y, Sun J M, Li S H, et al. Vertical variations of luminescence sensitivity of quartz grains from loess/paleosol of Luochuan section in the central Chinese Loess Plateau since the last interglacial[J]. Quaternary Geochronology, 2014, 22:107~115.

    Google Scholar

    赵华, 蒋复初, 卢演俦.郑州邙山马兰黄土的光释光(OSL)测年初步研究[J].地质力学学报, 1998, 4(4):19~29.

    Google Scholar

    ZHAO Hua, JIANG Fuchu, LU Yanchou. Preliminary study of OSL dating of the Malan loess at Mangshan Plateau, Zhengzhou, Henan Province[J]. Journal of Geomechanics, 1998, 4(4):19~29. (in Chinese with English abstract)

    Google Scholar

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