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Quaternary Stratigraphic Division and Sedimentary Characteristics of Borehole TB02 in the Southeast Margin of Beijing Plain, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2023年第01期
Page:
68-79
Research Field:
沉积地质与油气勘探
Publishing date:

Info

Title:
Quaternary Stratigraphic Division and Sedimentary Characteristics of Borehole TB02 in the Southeast Margin of Beijing Plain, China
Author(s):
NI Jing-bo1;  LIU Xiao2*;  ZHANG Xiao-liang1;  ZHANG Yue-ze1;  LIU Xiao-yong1;  YUAN Lu-peng3;  HE Fu-bing1
(1. Beijing Institute of Geological Survey, Beijing 102206, China; 2. Core and Samples Center of Natural Resources, China Geological Survey, Sanhe 065201, Hebei, China; 3. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China)
Keywords:
stratigraphic division;  sedimentary evolution;  AMS 14C dating;  magnetostratigraphy;  chronostratigraphy;  Quaternary;  grain size;  Beijing
PACS:
P533; P535
DOI:
10.19814/j.jese.2022.04014
Abstract:
Quaternary geology is important to the development of Quaternary resources and urban geological safety. The Quaternary geological borehole TB02 in Yongledian town, the southern Tongzhou district, Beijing was selected. Based on systematic core observation and cataloging, logging data analysis, the characteristics of grain size, together with AMS 14C and paleomagnetic dating, the chronostratigraphic division was carried out, and the sedimentary characteristics were discussed. The results show that the bottom of Quaternary is located at the depth of 276.21 m; the boundaries of Lower and Middle Pleistocene, and Middle and Upper Pleistocene are located at 97.75 and 39.32 m, respectively; the bottom of Holocene is located at the depth of 6.40 m. Grain size analysis shows that the sediments are mainly fine particle components, display good sorting properties, and present the characteristics of far-source deposition; the sedimentary hydrodynamic environment has changed significantly at 2 588, 1 539 and 781 ka for three times. Environmental evolution of the southeast margin of Beijing plain is as following: In the Early Pleistocene, the paleogeography sedimentary characteristics of the whole plain is dominated by stable lake sedimentary environment with weak hydrodynamic force; in the late stage of Early Pleistocene, the whole plain forms a braided river environment, and sufficient terrigenous detritus supply and strong construction capacity; since the Middle Pleistocene, the plain enters a peneplain process with weak hydrodynamic force and mainly fine-grained sediments, and the sedimentary geomorphology gradually finalizes, forming a broad plain area.

References:

[1] 罗明辉,张世民,任俊杰,等.北京断陷的新生代沉积与构造演化[C]∥中国地震局地壳应力研究所.地壳构造与地壳应力文集2008.北京:中国地震局地壳应力研究所,2008:62-74.
LUO Ming-hui,ZHANG Shi-min,REN Jun-jie,et al.Cenozoic Sedimentary and Tectonic Evolution in Beijing Down-warped Basin[C]∥Institute of Crustal Dynamics of China Earthquake Administration.Bulletin of Crustal Dynamics in 2008.Beijing:Institute of Crustal Dynamics of China Earthquake Administration,2008:62-74.
[2] 孙佳珺,孟勇琦,赵 帅.基于钻孔资料的北京平原区第四纪地层分析[J].中国矿业,2019,28(增1):107-110.
SUN Jia-jun,MENG Yong-qi,ZHAO Shuai.Quaternary Stratigraphic Analysis of the Beijing Plain Based on Drill Holes[J].China Mining Magazine,2019,28(S1):107-110.
[3] 王 永,闵隆瑞,董 进,等.河北白洋淀全新统沉积特征与地层划分[J].地球学报,2015,36(5):575-582.
WANG Yong,MIN Long-rui,DONG Jin,et al.Sedimentary Characteristics and Stratigraphic Division of Holocene Series in Baiyangdian,Hebei Province[J].Acta Geoscientia Sinica,2015,36(5):575-582.
[4] 袁路朋,王 永,姚培毅,等.河北雄县全新世中期海侵地层的发现[J].地质通报,2019,38(6):911-915.
YUAN Lu-peng,WANG Yong,YAO Pei-yi,et al.The Discovery of Mid-Holocene Transgressive Strata in Xiongxian County,Hebei Province[J].Geological Bulletin of China,2019,38(6):911-915.
[5] 杨彦峰,符超峰,徐新文,等.青藏高原东北缘尖扎盆地晚中新世地层绝对天文年代标尺的建立[J].地球科学与环境学报,2021,43(4):710-723.
YANG Yan-feng,FU Chao-feng,XU Xin-wen,et al.Establishment of Absolute Astronomical Time Scale of Late Miocene Strata of Jianzha Basin in the Northeastern Margin of Qinghai-Tibet Plateau,China[J].Journal of Earth Sciences and Environment,2021,43(4):710-723.
[6] 王 强,刘立军,徐海振,等.华北平原第四系下限的再研究[J].地质调查与研究,2003,26(1):52-60.
WANG Qiang,LIU Li-jun,XU Hai-zhen,et al.Re-study on the Lower Boundary of Quaternary System in the North China Plain[J].Geological Survey and Research,2003,26(1):52-60.
[7] 胡云壮,张金起,白耀楠,等.3.45 Ma以来滦河冲积扇中部唐山TD1孔记录的区域构造和气候演化[J].古地理学报,2014,16(2):249-262.
HU Yun-zhuang,ZHANG Jin-qi,BAI Yao-nan,et al.Records of Regional Tectonic and Climatic Evolution Since 3.45 Ma BP at Borehole TD1 of Tangshan in the Middle Part of Luanhe River Fluvial Fan[J].Journal of Palaeogeography,2014,16(2):249-262.
[8] 代 鹏,邓晓红,王盛栋,等.河北平原区固安G01孔岩心特征及第四纪地层划分[J].第四纪研究,2019,39(2):399-407.
DAI Peng,DENG Xiao-hong,WANG Sheng-dong,et al.Core Characteristics and Stratigraphic Classification of G01 Borehole in Gu'an,Hebei Plain[J].Quaternary Sciences,2019,39(2):399-407.
[9] 蔡向民,郭高轩,栾英波,等.北京山前平原区第四系三维结构调查方法研究[J].地质学报,2009,83(7):1047-1056.
CAI Xiang-min,GUO Gao-xuan,LUAN Ying-bo,et al.Quaternary Geological Features of Beijing Piedmont Plain Using 3-D Structural Method[J].Acta Geologica Sinica,2009,83(7):1047-1056.
[10] 安芷生,魏兰英,卢演俦,等.顺5孔的磁性地层学和早松山世的北京海侵[J].地球化学,1979,8(4):343-345.
AN Zhi-sheng,WEI Lan-ying,LU Yan-chou,et al.Magnetostratigraphy of the Core S-5 and the Transgression in the Beijing Area During the Early Matuyama Epoch[J].Geochimica,1979,8(4):343-346.
[11] 赵 勇,王 强,李瑞杰,等.北京平原区南部PGZ01孔第四纪地层划分及其环境意义[J].古地理学报,2018,20(2):337-348.
ZHAO Yong,WANG Qiang,LI Rui-jie,et al.Quaternary Stratigraphic Division and Its Environmental Significance of Borehole PGZ01 in Southern Beijing Plain Area[J].Journal of Palaeogeography,2018,20(2):337-348.
[12] 李瑞杰,赵 勇,魏 波,等.永定河中下游廊固凹陷北部ACX02钻孔地层年代学研究[J].地质力学学报,2019,25(2):249-256.
LI Rui-jie,ZHAO Yong,WEI Bo,et al.Stratigraphic Geochronology of ACX02 Borehole in the Middle and Lower Region of the Yongding River,the North of the Langgu Depression[J].Journal of Geomechanics,2019,25(2):249-256.
[13] 李鼎容,彭一民,刘清泗,等.北京平原区上新统—更新统的划分[J].地质科学,1979,14(4):342-351.
LI Ding-rong,PENG Yi-min,LIU Qing-si,et al.Subdivision of Pliocene-Pleistocene Series in Beijing Plain[J].Scientia Geologica Sinica,1979,14(4):342-351.
[14] 刘东生,丁梦林.中国第四纪地层和更新统、上新统界线[J].地层学杂志,1985,9(4):239-251.
LIU Dong-sheng,DING Meng-lin.Stratigraphic Boun-dary in China Between Quaternary and Pleistocene or Pliocene[J].Journal of Stratigraphy,1985,9(4):239-251.
[15] 李龙吟,陈华慧.北京怀柔地区第四纪下限的综合标志[J].地球科学,1992,17(6):631-637.
LI Long-yin,CHEN Hua-hui.Comprehensive Criteria for the N/Q Boundary in Huairou Area,Beijing,China[J].Earth Science,1992,17(6):631-637.
[16] 梅 枭,孙洪艳,武法东,等.中国第四纪下限研究现状浅析[J].地质论评,2014,60(4):741-747.
MEI Xiao,SUN Hong-yan,WU Fa-dong,et al.An Analysis on the Situation of the Lower Boundary of Quaternary Period in China[J].Geological Review,2014,60(4):741-747.
[17] 贾 婷,王 永,浦庆余,等.中国第四纪下限问题研究综述[J].地质力学学报,2016,22(1):162-177.
JIA Ting,WANG Yong,PU Qing-yu,et al.Review on the Lower Boundary of Quaternary in China[J].Journal of Geomechanics,2016,22(1):162-177.
[18] 徐锡伟,白鸾曦,魏雷鸣,等.华北克拉通破坏区最新构造运动起始时间讨论[J].地球科学,2019,44(5):1647-1660.
XU Xi-wei,BAI Luan-xi,WEI Lei-ming,et al.Discussion on Initiation Time of the Latest Tectonic Movement in Break-up Region of the North China Craton[J].Earth Science,2019,44(5):1647-1660.
[19] KRUMBEIN W C.Size Frequency Distributions of Sediments[J].Journal of Sedimentary Research,1934,4(2):65-77.
[20] FOLK R L,WARD W C.Brazos River Bar:A Study in the Signification of Grain Size Parameters[J].Journal of Sedimentary Petrology,1957,27(1):3-27.
[21] REIMER P J,AUSTIN W E N,BARD E,et al.The IntCal20 Northern Hemisphere Radiocarbon Age Ca-libration Curve(0-55 kcal BP)[J].Radiocarbon,2020,62(4):725-757.
[22] SINGER B S.A Quaternary Geomagnetic Instability Time Scale[J].Quaternary Geochronology,2014,21(1):29-52.
[23] 程天赦,杨文静,代 鹏,等.永定河冲洪积平原南部QHJ01孔第四纪地层划分及其环境意义[J].华北地质,2021,44(4):47-54.
CHENG Tian-she,YANG Wen-jing,DAI Peng,et al.Quaternary Stratigraphic Division and Its Environmental Significance of Borehole QHJ01 in Southern Alluvial Plain of the Yongding River[J].North China Geology,2021,44(4):47-54.
[24] LI Y,SONG Y G,LAI Z P,et al.Rapid and Cyclic Dust Accumulation During MIS 2 in Central Asia Inferred from Loess OSL Dating and Grain-size Analysis[J].Scientific Reports,2016,6:32365.
[25] JIANG H C,WANG P,THOMPSON J,et al.Last Glacial Climate Instability Documented by Coarse-grained Sediments Within the Loess Sequence,at Fanjiaping,Lanzhou,China[J].Quaternary Research,2009,72(1):91-102.
[26] 何继山,梁 杏,李 静,等.天津滨海平原区深孔沉积物环境敏感粒度提取及其意义[J].地球科学,2015,40(7):1215-1225.
HE Ji-shan,LIANG Xing,LI Jing,et al.Environmentally Sensitive Grain-size Extraction of Deep Hole Sediment from Tianjin Coastal Plain and Its Significance[J].Earth Science,2015,40(7):1215-1225.
[27] 赵红梅,刘林敬,赵 华,等.滹沱河古河道剖面粒度参数特征及沉积环境[J].现代地质,2016,30(2):485-492.
ZHAO Hong-mei,LIU Lin-jing,ZHAO Hua,et al.Grain Size Character and Sedimentary Environment of Hutuo River Paleochannel Section[J].Geoscience,2016,30(2):485-492.
[28] 田 飞,王 永,迟振卿,等.内蒙古东南缘晚第四纪以来的气候环境演化[J].地质力学学报,2017,23(4):602-611.
TIAN Fei,WANG Yong,CHI Zhen-qing,et al.Later Quaternary Climatic and Environmental Changes in the Southeastern Margin of Inner Mongolia[J].Journal of Geomechanics,2017,23(4):602-611.
[29] 张 璞,陈建强,田明中,等.沉积物粒度分析在厦门市第四纪环境研究和地层划分对比中的应用[J].地球科学与环境学报,2005,27(1):88-94.
ZHANG Pu,CHEN Jian-qiang,TIAN Ming-zhong,et al.Application of Sediments Grain Size Analysis in Quaternary Environmental Research and Its Stratum Compartmentalization and Contrast Function in Xiamen Island,Fujian Province[J].Journal of Earth Sciences and Environment,2005,27(1):88-94.
[30] 田 飞,王 永,袁路朋,等.浑善达克沙地碱湖表层沉积物的粒度、沉积有机质变化特征与指示意义[J].地学前缘,2022,29(2):317-326.
TIAN Fei,WANG Yong,YUAN Lu-peng,et al.Surface Sediments of an Alkaline Lake in the Otindag Sandy Land:Grain Size and Sedimentary Organic Matter Variations and Their Environmental Significance[J].Earth Science Frontiers,2022,29(2):317-326.
[31] 蒋庆丰,刘兴起,沈 吉.乌伦古湖沉积物粒度特征及其古气候环境意义[J].沉积学报,2006,24(6):877-882.
JIANG Qing-feng,LIU Xing-qi,SHEN Ji.Grain-size Characteristics of Wulugu Lake Sediments and Its Palaeoclimate and Palaeoenvironment Implication[J].Acta Sedimentologica Sinica,2006,24(6):877-882.
[32] 赵淑君,程 捷,尹功明,等.北京平原区中更新世以来的孢粉组合及其古气候意义[J].古地理学报,2008,10(6):637-646.
ZHAO Shu-jun,CHENG Jie,YIN Gong-ming,et al.Palynological Assemblages and Paleoclimatic Significance in Beijing Plain Area Since the Middle Pleistocene[J].Journal of Palaeogeography,2008,10(6):637-646.
[33] 蔡向民,郭高轩,张 磊,等.北京城湖泊的成因[J].中国地质,2013,40(4):1092-1098.
CAI Xiang-min,GUO Gao-xuan,ZHANG Lei,et al.The Origin of Lakes in Beijing City[J].Geology in China,2013,40(4):1092-1098.
[34] 刘晓燕,袁四化,刘智荣,等.北京平原东北部晚更新世晚期金鸡河一级阶地孢粉记录[J].科学技术与工程,2015,15(33):5-9.
LIU Xiao-yan,YUAN Si-hua,LIU Zhi-rong,et al.Sporopollen Record in Jinji River Level Terrace During the Late Late Pleistocene in Northeast Beijing Plain[J].Science Technology and Engineering,2015,15(33):5-9.

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Last Update: 2023-01-30