Volume 29 Issue 1
Feb.  2023
Turn off MathJax
Article Contents
CHEN H Q,ZHUAN S P,ZHAO H P,et al.,2023. Evolution and changes of the ancient Luanhe fluvial fan since the Quaternary in Tangshan, Hebei Province[J]. Journal of Geomechanics,29(1):138−152 doi: 10.12090/j.issn.1006-6616.2022023
Citation: CHEN H Q,ZHUAN S P,ZHAO H P,et al.,2023. Evolution and changes of the ancient Luanhe fluvial fan since the Quaternary in Tangshan, Hebei Province[J]. Journal of Geomechanics,29(1):138−152 doi: 10.12090/j.issn.1006-6616.2022023

Evolution and changes of the ancient Luanhe fluvial fan since the Quaternary in Tangshan, Hebei Province

doi: 10.12090/j.issn.1006-6616.2022023
Funds:  This research is financially supported by the Geological Survey Program of the China Geological Survey (Grant No. DD20160042), the Fundamental Geology Survey Program of the China Geological Survey (Grant No. DD20160060), the Comprehensive Research Program of the China Geological Survey (Grant No. DD20179394), and the Comprehensive Research Program of Hebei Bureau of Geology and Mineral Resources Exploration (Grant No. 201821).
More Information
  • Received: 2022-02-25
  • Revised: 2022-11-20
  • Available Online: 2022-08-06
  • The study of the ancient Luanhe alluvial fan has focused more on the Holocene, and no systematic study has been conducted on its Pleistocene evolution and variation. We studied the magnetic stratigraphy, chronostratigraphy, sedimentology, logging sedimentology, and core color of the boreholes PZK10 and PZK20 in the ancient Luanshe alluvial fan. Based on that, we carried out a comprehensive study of the Quaternary three-dimensional geological structure, the scale of the alluvial fan body, and the migration pattern of the ancient Luanshe alluvial plain. The borehole PZK10 recorded Brunches, Matuyama, and Gauss polarity chrons; the boundaries between them are 77.42 m and 71.50 m, respectively. The borehole PZK10 also revealed a set of diluvial “mud-gravel” layers deposited in the Pliocene, with two alluvial fan-lake phase cycles in the Early Pleistocene, braided river deposits in the Middle Pleistocene, and lake, alluvial fan and braided river facies in the late Pleistocene. A set of highly thick “mud-gravel” layers was deposited in the Pliocene of the borehole PZK20. The early Pleistocene is the fan-front–plain-braided river facies deposition, the middle Pleistocene is the braided river–alluvial fan facies deposition, and the late Pleistocene is the braided river deposition. Early Pleistocene, the ancient Luanhe River out of the mountain formed a large-scale alluvial fan in Shaliuhe town, which is the first stage of the ancient Luanhe alluvial fan. In the middle of the early Pleistocene, the ancient Luanhe River diverged in the current Qiuzhuang reservoir, and the alluvial fan formed in the Fengrun area, namely the second stage alluvial fan. In the middle Pleistocene, the first alluvial fan began to shrink, while the second alluvial fan continued to develop, forming a vast thick gravel layer. Late Pleistocene, the ancient Luanhe river was captured north of Qianxi county. It flowed eastwards and migrated out of the research area into the Qian’an basin in Xixiakou village, forming the alluvial fan with Xixiakou village as its apex.

     

  • Full-text Translaiton by iFLYTEK

    The full translation of the current issue may be delayed. If you encounter a 404 page, please try again later.
  • loading
  • CANDE S C, KENT D V, 1995. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic[J]. Journal of Geophysical Research: Solid Earth, 100(B4): 6093-6095. doi: 10.1029/94JB03098
    CHEN H Q, ZHUAN S P, CHEN C, et al. , 2021. Quaternary activity of the Fengtai-Yejituo fault in Tangshan, Hebei Province: evidence from 14C and magnetic stratigraphy[J]. Geology in China, 48(2): 605-617. (in Chinese with English abstract)
    FANG X M, XI X X, LI J J, et al. , 1997. Discovery of the late Miocene climate change and its significance in Western China[J]. Chinese Science Bulletin, 42(23): 2521-2524. (in Chinese) doi: 10.1360/csb1997-42-23-2521
    GAO S M, 1981. Facies and sedimentary model of the Luan Riverdelta[J]. Acta Geographica Sinica, 36(3): 303-314. (in Chinese with English abstract)
    GAO S M, 1982. Supplement new recognition on Luanhe River delta[J]. Acta Geographica Sinica, 37(4): 424-426. (in Chinese)
    GAO S M, 1985. Structures and sedimentary environments of the alluvial fan of the Luan River[J]. Geographical Research, 4(1): 54-62. (in Chinese with English abstract)
    Geological Insititute of Dagang Oil Field, Bureau of Marine Petroleum Exploration, Institute of Marine Geology, Tongji University, 1985. The Luanhe River alluvial fan-delta[M]. Beijing: Geological Publishing House: 1-164. (in Chinese)
    HU Y Z, ZHANG J Q, BAI Y N, et al. , 2014. 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, 16(2): 249-262. (in Chinese with English abstract)
    KIRSCHVINK J L, 1980. The least-squares line and plane and the analysis of palaeomagnetic data[J]. Geophysical Journal International, 62(3): 699-718. doi: 10.1111/j.1365-246X.1980.tb02601.x
    LI C X, CHEN G, WANG C G, et al. , 1984. On the Luanhe river alluvial fan-delta complex[J]. Acta Petrolei Sinica, 5(4): 27-36. (in Chinese with English abstract)
    LI C X, WANG Q, FAN D D, 2013. Oceanic delta[C]//Sedimentology of China. Beijing: Petroleum Industry Press: 812-905. (in Chinese)
    LI Y, 1987. Mechanism of the appearance of Fengrun-Fengtai concealed active fault on Landsat image[J]. Journal of Seismology, 21(1): 39-42. (in Chinese with English abstract)
    LI Y F, GAO S M, AN F T, 1982. A preliminary study of the Quaternary marine strata and its Paleogeographic significance in the Luanhe delta region[J]. Oceanologia et Limnologia Sinica, 13(5): 433-439. (in Chinese with English abstract)
    LIN X, LIU J, WU Z H, et al. , 2021. Study on borehole provenance tracing and fluvial sediment diffusion in the Bohai Sea: double constraints from detrital zircon U-Pb age and in-situ geochemical element of apatite grains[J]. Journal of Geomechanics, 27(2): 304-316. (in Chinese with English abstract)
    MA Z, 1982. Utilization of the combination of log shapes for explanation of the sedimentary environment[J]. Oil & Gas Geology, 3(1): 25-40. (in Chinese with English abstract)
    QIN B C, FANG W X, ZHANG J G, et al. , 2021. Quaternary sedimentary sequence and sedimentary environment restoration in the Jinzhong Basin, Fenhe Rift Valley[J]. Journal of Geomechanics, 27(6): 1035-1050. (in Chinese with English abstract)
    Regional Geological and Mineral Resources Survey Institute of Hebei Province, 2017. The regional geology of China, Hebei Province[M]. Beijing: Geological Publishing House: 1-1272. (in Chinese)
    SHEN J, ZHANG E L, XIA W L, 2001. Records From lake sediments of the Qinghai lake to mirror climatic and environmental changes of the past about 1000 years[J]. Quaternary Sciences, 21(6): 508-513. (in Chinese with English abstract)
    SONG F, HOU J G, ZHANG Z, et al. , 2009. Application of log curves in indicating sedimentary micro-facies of lake facies basins[J]. Well Logging Technology, 33(6): 589-592. (in Chinese with English abstract)
    WANG J R, LIU H T, 2004. Identification of sedimentary microfacies of logging and its application[J]. Journal of Daqing Petroleum Institute, 28(4): 18-20. (in Chinese with English abstract)
    WANG N A, LI J J, CAO J X, et al. , 1999. A preliminary research on the climatic records of lacustrine deposits of Qingtu Lake in the last 6000 years[J]. Scientia Geographica Sinica, 19(2): 119-124. (in Chinese with English abstract)
    WANG P X, MIN Q B, BIAN Y H, et al. , 1981. Strata of quaternary transgressions in East China: a preliminary study[J]. Acta Geological Sinica, 55(1): 1-13. (in Chinese with English abstract)
    WANG Q, TIAN G Q, 1999. The neotectonic setting of late Quaternary transgressions on the Eastern coastal plain of China[J]. Journal of Geomechanics, 5(4): 41-48. (in Chinese with English abstract)
    WANG Q, LI C X, 2009. The type of quaternary sequence in the East China coastal plain[J]. Marine Geology & Quaternary Geology, 29(4): 39-51. (in Chinese with English abstract)
    WANG Q, ZHANG Y F, YUAN G B, et al. , 2008. Since MIS 3 stage the correlation between transgression and climatic changes in the North Huanghua area, Hebei[J]. Quaternary Sciences, 28(1): 79-95. (in Chinese with English abstract)
    WU C, 1984. Surface ancient channels in Hebei Plain[J]. Acta Geographica Sinica, 39(3): 268-276. (in Chinese with English abstract)
    WU Y H, LI S J, 2004. Significance of lake sediment color for short time scale climate variation[J]. Advances in Earth Science, 19(5): 789-792. (in Chinese with English abstract)
    XU J, MA Z J, CHEN G G, et al. , 2005. Estimating times of quaternary tectonic episodes in the Bohai sea based on Geomorphic features of surrounding mountainous areas[J]. Quaternary Sciences, 25(6): 700-710. (in Chinese with English abstract)
    XU L, MIAO Y F, FANG X M, et al. , 2009. Middle Eocene-Oligocene climatic changes recorded by sedimentary colors in the Xining Basin, in northeastern Tibetan Plateau, NW China[J]. Journal of Lanzhou University (Natural Sciences), 45(1): 12-19. (in Chinese with English abstract)
    XU Q M, YUAN G B, ZHANG J Q, et al. , 2011. Stratigraphic division of the late Quaternary strata along the coast of Bohai Bay and its geology significance[J]. Acta Geologica Sinica, 85(8): 1352-1367. (in Chinese with English abstract)
    XUE C T, 2016. Extents, type and evolution of Luanhe river fan-delta system, China[J]. Marine Geology & Quaternary Geology, 36(6): 13-22. (in Chinese with English abstract)
    ZHAO L L, XU Q M, YANG J L, et al. , 2016. Sedimentary evolution of BG10 borehole in northern coast of Bohai Bay during Late Cenozoic[J]. Quaternary Sciences, 36(1): 196-207. (in Chinese with English abstract)
    陈宏强, 专少鹏, 陈超, 等, 2021. 河北省唐山地区丰台-野鸡坨断裂第四纪活动性—来自14C和磁性地层年代学的证据[J]. 中国地质, 48(2): 605-617.
    大港油田地质研究所, 海洋石油勘探局研究院, 同济大学海洋地质研究所, 1985. 滦河冲积扇-三角洲沉积体系[M]. 北京: 地质出版社: 1-164.
    方小敏, 奚晓霞, 李吉均, 等, 1997. 中国西部晚中新世气候变干事件的发现及其意义[J]. 科学通报, 42(23): 2521-2524.
    高善明, 1981. 全新世滦河三角洲相和沉积模式[J]. 地理学报, 36(3): 303-314. doi: 10.3321/j.issn:0375-5444.1981.03.006
    高善明, 1982. 对滦河三角洲一些补充和再认识[J]. 地理学报, 37(4): 424-426. doi: 10.3321/j.issn:0375-5444.1982.04.009
    高善明, 1985. 滦河冲积扇结构和沉积环境[J]. 地理研究, 4(1): 54-62.
    河北省区域地质矿产调查研究所, 2017. 中国区域地质志·河北志[M]. 北京: 地质出版社: 1-1272.
    胡云壮, 张金起, 白耀楠, 等, 2014. 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, 16(2): 249-262.
    李从先, 陈刚, 王传广, 等, 1984. 论滦河冲积扇-三角洲沉积体系[J]. 石油学报, 5(4): 27-36.
    李从先, 王强, 范代读, 2013. 海洋三角洲[C]//中国沉积学. 北京: 石油工业出版社: 812-905.
    李勇, 1987. 丰润-丰台隐伏活动断裂在卫星影象上的表现机制[J]. 地震学刊, 21(1): 39-42.
    李元芳, 高善明, 安凤桐, 1982. 滦河三角洲地区第四纪海相地层及其古地理意义的初步研究[J]. 海洋与湖沼, 13(5): 433-439.
    林旭, 刘静, 吴中海, 等, 2021. 渤海钻孔物源示踪和河流沉积物扩散研究: 碎屑锆石U-Pb年龄和磷灰石原位地球化学元素双重约束[J]. 地质力学学报, 27(2): 304-316.
    马正, 1982. 应用自然电位测井曲线解释沉积环境[J]. 石油与天然气地质, 3(1): 25-40. doi: 10.11743/ogg19820103
    秦帮策, 方维萱, 张建国, 等, 2021. 汾河裂谷晋中盆地内第四纪沉积序列与沉积环境恢复[J]. 地质力学学报, 27(6): 1035-1050.
    沈吉, 张恩楼, 夏威岚, 2001. 青海湖近千年来气候环境变化的湖泊沉积记录[J]. 第四纪研究, 21(6): 508-513.
    宋璠, 侯加根, 张震, 等, 2009. 利用测井曲线研究陆相湖泊沉积微相[J]. 测井技术, 33(6): 589-592. doi: 10.3969/j.issn.1004-1338.2009.06.020
    天津市地质调查研究院, 河北省地质调查院, 2005. 1: 25万天津市幅区域地质调查报告[R].
    王金荣, 刘洪涛, 2004. 测井沉积微相识别方法及应用[J]. 大庆石油学院学报, 28(4): 18-20.
    王乃昂, 李吉均, 曹继秀, 等, 1999. 青土湖近6000年来沉积气候记录研究: 兼论四五世纪气候回暖[J]. 地理科学, 19(2): 119-124.
    汪品先, 闵秋宝, 卞云华, 等, 1981. 我国东部第四纪海侵地层的初步研究[J]. 地质学报, 55(1): 1-13.
    王强, 田国强, 1999. 中国东部晚第四纪海侵的新构造背景[J]. 地质力学学报, 5(4): 41-48.
    王强, 张玉发, 袁桂邦, 等, 2008. MIS 3阶段以来河北黄骅北部地区海侵与气候期对比[J]. 第四纪研究, 28(1): 79-95. doi: 10.3321/j.issn:1001-7410.2008.01.009
    王强, 李从先, 2009. 中国东部沿海平原第四系层序类型[J]. 海洋地质与第四纪地质, 29(4): 39-51.
    吴忱, 1984. 河北平原的地面古河道[J]. 地理学报, 39(3): 268-276.
    吴艳宏, 李世杰, 2004. 湖泊沉积物色度在短尺度古气候研究中的应用[J]. 地球科学进展, 19(5): 789-792. doi: 10.3321/j.issn:1001-8166.2004.05.016
    徐杰, 马宗晋, 陈国光, 等, 2005. 根据周围山地第四纪地貌特征估计渤海第四纪构造活动幕的发生时间[J]. 第四纪研究, 25(6): 700-710.
    徐丽, 苗运法, 方小敏, 等, 2009. 青藏高原东北部西宁盆地中始新世-渐新世沉积物颜色与气候变化[J]. 兰州大学学报(自然科学版), 45(1): 12-19.
    胥勤勉, 袁桂邦, 张金起, 等, 2011. 渤海湾沿岸晚第四纪地层划分及地质意义[J]. 地质学报, 85(8): 1352-1367.
    薛春汀, 2016. 滦河冲积扇-三角洲的范围和类型及其演化[J]. 海洋地质与第四纪地质, 36(6): 13-22. doi: 10.16562/j.cnki.0256-1492.2016.06.003
    赵琳琳, 胥勤勉, 杨吉龙, 等, 2016. 渤海湾北岸BG10孔晚新生代沉积环境演化过程[J]. 第四纪研究, 36(1): 196-207. doi: 10.11928/j.issn.1001-7410.2016.19
  • 加载中

Catalog

    Figures(9)  / Tables(2)

    Article Metrics

    Article views (651) PDF downloads(81) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return