Stratigraphy and sedimentary facies of Borehole ACX03 at Langgu sag in Hebei Plain since the Late Pliocene
Li Rui-Jie1, Wang Qiang2, Zhao Yong1, Wei Bo1, Sun Yong-Hua1
1 Beijing Institute of Geological Survey,Beijing 100195,China; 2 Tianjin Center of Geological Survey, China Geological Survey(CGS),Tianjin 300170,China
Abstract Base on the 14C age and magnetic stratigraphy of Borehole ACX03 with the depth of 300.0 m,and is located in the northeast part of Langgu sag,Hebei Plain,the Quaternary stratigraphic framework of borehole was established. Based on the core sediment, logging curves and micropaleontological characteristics,the paper divided sedimentary intervals and analyzed sedimentary environment of Borehole ACX03. The results show that: the B/M and M/G polarity boundaries of Borehole ACX03 are located at 83.8 m and 220.2 m,the age of the hole bottom is about 3.2 Ma,13 sedimentary intervals was divided. The Pliocene(220.2~300.0 m)in Borehole ACX03 was river and floodplain deposit which mingle Lakes deposit,the Lower Pleistocene(85.2~220.2 m)was river,lake and floodplain deposit,the middle Pleistocene(61.5~85.2 m)was branched channel deposit which mingle floodplain and interfluvial-limnetic deposit,the Upper Pleistocene(23.2~61.5 m)was floodplain and branched channel deposit,and the Holocene(0~23.2 m)was flood plain and curved-oxbow lake deposits. Comparison of the Quaternary strata of Borehole ACX03 and adjacent boreholes shows that the differential subsidence of the early Pleistocene is strongest,and then it gets weaker and weaker until the Holocene in Langfang-Gu’an area of Hebei Plain.
Fund:Regional Geological Survey Project of China Geological Survey(No.12120114007701),Beijing Geological Survey Project(No. PXM2019-158203-000005)and the National Natural Science Foundation of China(No.40872107)
Corresponding Authors:
Wang Qiang,born in 1945,is a professor of Tianjin Center of Geological Survey(CGS). He is mainly engaged in Quaternary geology and marine geology. E-mail: tjwq1945@163.com.
About author: Li Rui-Jie,born in 1988,is an engineer of Beijing Institute of Geological Survey. He is mainly engaged in regional geology research. E-mail: wylrj163@163.com.
Cite this article:
Li Rui-Jie,Wang Qiang,Zhao Yong et al. Stratigraphy and sedimentary facies of Borehole ACX03 at Langgu sag in Hebei Plain since the Late Pliocene[J]. JOPC, 2021, 23(3): 539-554.
Li Rui-Jie,Wang Qiang,Zhao Yong et al. Stratigraphy and sedimentary facies of Borehole ACX03 at Langgu sag in Hebei Plain since the Late Pliocene[J]. JOPC, 2021, 23(3): 539-554.
[1] 蔡向民,郭高轩,栾英波,孙知明,梁亚楠,姜龙群. 2010. 永定河形成时代研究. 第四纪研究, 30(1): 167-174. [Cai X M,Guo G X,Luan Y B,Sun Z M,Liang Y N,Jiang L Q.2010. Forming time for the Yongdinghe River. Quaternary Sciences, 30(1): 167-174] [2] 代鹏,邓晓红,王盛栋,武军杰,张全. 2019a. 河北平原区固安G01孔岩心特征及第四纪地层划分. 第四纪研究, 39(2): 399-407. [Dai P,Deng X H,Wang S D,Wu J J,Zhang Q.2019a. Core characteristics and stratigraphic classification of G01 Borehole in Gu’an,Hebei Plain. Quaternary Sciences, 39(2): 399-407] [3] 代鹏,王盛栋,邓晓红,武军杰,张全,荣立新,刘东明. 2019b. 地球物理方法在厚覆盖区第四纪地层划分中的应用. 地球物理学进展, 34(6): 2143-2151. [Dai P,Wang S D,Deng X H,Wu J J,Zhang Q,Rong L X,Liu D M.2019b. The application of geophysical methods in the Quaternary stratigraphic division of thick covered area. Progress in Geophysics, 34(6): 2143-2151] [4] 陈望和,倪明云,等. 1987. 河北第四纪地质. 北京: 地质出版社,78-170. [Chen W H,Ni M Y,et al.1987. Quaternary Geology of Hebei. Beijing: Geological Publishing House,78-170] [5] 胡云壮,张金起,白耀楠,夏雨波,王强. 2014a. 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. 古地理学报, 16(2): 249-262. [Hu Y Z,Zhang J Q,Bai Y N,Xia Y P,Wang Q.2014a. Records of regional tectonica and climatec evolution since 3.45 Ma BP at Borehole TD1 of Tangshan in middle part of Luanhe River fluvial fan. Journal of Palaeogeography(Chinese Edition), 16(2): 249-262] [6] 胡云壮,胥勤勉,袁桂邦,裴军令,杨吉龙,张玉发,王强. 2014b. 河北海兴小山CK3孔磁性地层与第四纪火山活动记录. 古地理学报, 16(3): 411-426. [Hu Y Z,Xu Q M,Yuan G B,Pei J L,Yang J L,Zhang Y F,Wang Q.2014b. Magnetostratigraphy of Borehole CK3 and record of the Quaternary volcanic activities in Xiaoshan of Haixing,Hebei Province. Journal of Palaeogeography(Chinese Edition), 16(3): 411-426] [7] 李从先,汪品先. 1998. 长江晚第四纪河口地层学研究. 北京: 科学出版社,50-122. [Li C X,Wang P X, et al.1998. Late Quaternary Estuary Stratigraphy of the Changjiang(Yangtze)Delta. Beijing: Science Press,50-122] [8] 李瑞杰,赵勇,魏波,孙永华,王强. 2019. 永定河中下游廊固凹陷北部钻孔地层年代学研究. 地质力学学报, 25(2): 249-256. [Li R J,Zhao Y,Wei B,Sun Y H,Wang Q.2019. Stratigraphic geochronology of ACX2 Borehole in the middle and lower region of the Yongdinghe River,the north of the Lang’gu Depression. Journal of Geomechanics, 25(2): 249-256] [9] 李天杰,郑应顺,王云. 1983. 土壤地理学(第二版).北京: 高等教育出版社,113-135. [Li T J,Zheng Y S,Wang Y.1983. Soil Geography(Second Edition). Beijing: Higher Education Press,113-135] [10] 刘国臣,陆克政,严俊君. 1996. 廊固凹陷构造特征及成因解析. 地质论评,42(S1): 83-88. [Liu G C,Lu K Z,Yan J J.1996. Structural characteristics and genetic analysis of Langgu depression. Geological Review,42(S1): 83-88] [11] 鲁庆伟,王强,詹健,郭维,李稳,王西玉. 2018. 渤海湾西岸沧县隆起中更新世地层间断. 古地理学报, 20(4): 665-679. [Lu Q W,Wang Q,Zhan J,Guo W,Li W,Wang X Y.2018. Middle Pleistocene stratigraphic hiatus on the Cangxian Uplift,the west coast of Bohai Bay. Journal of Palaeogeography(Chinese Edition), 20(4): 665-679] [12] 马正. 1982. 应用自然电位测井曲线解释沉积环境. 石油与天然气地质, 3(1): 25-40. [Ma Z.1982. Utilization of the combination of log shapes for explanation of the sedimentary environment. Oil & Gas Geology, 3(1): 25-40] [13] 孙振营,王强,李亚平,裴军令,周相国,高学飞. 2018. 第四纪以来天津北部燕山隆升与山前盆地的形成. 古地理学报, 20(5): 893-908. [Sun Z Y,Wang Q,Li Y P,Pei J L,Zhou X G,Gao X F.2018. The uplift of Yanshan Mountain and the formation of piedmont basin in northern Tianjin since the Quaternary. Journal of Palaeogeography(Chinese Edition), 20(5): 893-908] [14] 王强. 1982. 渤海湾西岸海相与海陆过渡相介形类动物群与古地理. 海洋地质研究, 2(3): 36-46. [Wang Q.1982. The ostracod fauna of marine and marine-terrestrial transitional facies in western coast of the Bohai Gulf(North China)and paleogeography during Quaternary. Marine Geological Research, 2(3): 36-46] [15] 王强,王景哲. 1988. 中国第四纪介形虫动物群. 见: 中国地层(14),中国的第四系. 北京: 地质出版社,214-226. [Wang Q,Wang J Z.1988. Quaternary ostracoda fauna in China. In: Stratigraphy in China(14),The Quaternary System of China. Beijing: Geological Publishing House,214-226] [16] 王强,宋大伟,王云生. 1992. 第七章第四系. 见: 邓永高(主编).中华人民共和国地质矿产部地质专报,一,区域地质,第 29号: 天津市区域地质志. 北京: 地质出版社,116-156. [Wang Q,Song D W,Wang Y S.1992. 7th Chapter,Quaternary System. In: Deng Y G(ed). PR China,Ministry of Geol. & Min.Res.,Geol.Memoirs,ser.1,No.29,Regional Geology of Tianjin Municipality. Beijing: Geological Publishing House,116-156] [17] 王强,吕金福. 1995. 海面变化与海岸变迁. 见: 李汉鼎,吕金福,王强,等. 中国北方沿海泥炭与环境. 北京: 海洋出版社,109-128. [Wang Q,Lü J F.1995. Eustacy and coastline movement. In: Li H D,Lü J F,Wang Q et al.(eds). Peat and Environment on Coastal Area of the North China. Beijing: China Ocean Press,109-128] [18] 王强,郭盛乔. 1999. 华北平原古气候演化与古环境重塑. 见: 张宗祜等. 中国北方晚更新世以来地质环境演化与未来生存环境变化趋势预测. 北京: 地质出版社,59-98. [Wang Q,Guo S Q.1999. Palaeoclimatic change and palaoenvironment reconstruct.In: Zhang Z H et al(eds).Geological Environment Change and Trend Prodiction of Future Living Environment. Beijing: Geological Publishing House,59-98] [19] 王强,田国强. 1999. 中国东部晚第四纪海侵的新构造背景. 地质力学学报, 4(4): 42-48. [Wang Q,Tian G Q.1999. The neotectonic settings of late Quaternary transgression on the eastern coastal plain of China. Journal of Geomechanics, 4(4): 42-48] [20] 王强,刘立军,徐海振,马震,职太平,兰自亭,王亚斌,刘雪松,林沛,董殿伟. 2003. 华北平原第四系下限的再研究. 地质调查与研究, 26(1): 52-60. [Wang Q,Liu L J,Xu H Z,Ma Z,Zhi T P,Lan Z T,Wang Y B,Liu X S,Lin P,Dong D W.2003. Re-study on the lower boundary of Quaternary system in the North China Plain. Geological Survey and Research, 26(1): 52-60] [21] 王强,李从先. 2009. 中国东部沿海平原第四系层序类型. 海洋地质与第四纪地质, 29(4): 39-51. [Wang Q,Li C X.2009. The type of Quaternary sequence in the East China coastal plain. Marine Geology & Quaternary Geology, 29(4): 39-51] [22] 王强. 2019. 天津—河北沿海钻孔地层中的末次盛冰期下切河谷. 地质力学学报, 25(5): 877-889. [Wang Q.2019. Insized valley of Last Glacial Maximum Stage in the drilling strata on the Tianjin-Hebei coastal plain. Journal of Geomechanics, 25(5): 877-889] [23] 王忠蕾,郑洪波,梅西,孟祥君,强小科. 2020. 辽东湾北部钻孔磁性地层年代框架及地质意义. 第四纪研究, 40(3): 616-632. [Wang Z L,Zheng H B,Mei X,Meng X J,Qiang X K.2020. Magnetic stratigraphy of boreholes in the north of Liaodong Bay and its significance. Quaternary Sciences, 40(3): 616-632] [24] 田建章,苏建杰,辛玮江,丛良滋,曹建华,徐玉萍,田会琴. 2012. 廊固凹陷潜山成藏模拟及油气勘探潜力. 中国石油勘探, 17(6): 53-57. [Tian J Z,Su J J,Xin W J,Cong L Z,Cao J H,Xu Y P,Tian H Q.2012. Buried hill accumulation model and oil and gas exploration potential in Langgu Depression. China Petroleum Exploration, 17(6): 53-57] [25] 谢叶彩,王强,龙桂,周洋,郑志敏,黄雪飞. 2014. 珠江口小榄镇—万顷沙地区晚更新世以来的海侵层序. 古地理学报, 16(6): 835-852. [Xie Y C,Wang Q,Long G,Zhou Y,Zheng Z M,Huang X F.2014. Transgressive sequence since the Late Pleistocene in Xiaolan Town Wanqingsha area,Zhujiang River estuary. Journal of Palaeogeography(Chinese Edition), 16(6): 835-852] [26] 杨明慧,刘池洋,杨斌谊,赵红格. 2002. 冀中坳陷古近纪的伸展构造. 地质论评, 48(1): 58-65. [Yang M H,Liu C Y,Yang B Y,Zhao H G.2002. Extensional structures of the Paleogene in the central Hebei Basin,China. Geological Review, 48(1): 58-65] [27] 袁宝印,邓成龙,吕金波,金昌柱,吴玉书. 2002. 北京平原晚第四纪堆积期与史前大洪水. 第四纪研究, 22(5): 474-480. [Yuan B Y,Deng C L,Lü J B,Jin C Z,Wu Y S.2002. A Late Quaternary accumulation period and the prehistoric flood in Beijing plain. Quaternary Sciences, 22(5): 474-480] [28] 张丹丹,戴俊生,邹娟,王珂. 2014. 冀中坳陷廊固凹陷古近纪断层活动特征. 地质力学学报, 20(1): 25-33. [Zhang D D,Dai J S,Zou J,Wang K.2014. Research on fault activity in Paleogene of Langgu Sag,Jizhong Depression. Journal of Geomechanics, 20(1): 25-33] [29] 张广权,李浩,胡向阳,陈舒薇,高阳. 2018. 一种利用测井曲线齿化率刻画河道的新方法. 天然气地球科学, 29(12): 1767-1774. [Zhang G Q,Li H,HU X Y,Chen S W,Gao Y.2018. Study of the method of the portrayed the river by calculating the tooth rate of logging curve. Natural Gas Geoscience, 29(12): 1767-1774] [30] 张青松,李元芳,邢嘉明,濮静娟. 1976. 水系变迁与新构造运动: 以北京平原地区为例. 地理集刊, 第10号: 71-82. [Zang Q S,Li Y F,Xing J M,Pu J J.1976. Water system changes and neotectonic movement: take the Beijing Plain area for example. Geography Memoirs,No.10: 71-82] [31] 赵勇,王强,李瑞杰,魏波,徐吉祥,孙永华,张晓亮,王纯君,周圆心,尤世娜,吕金波. 2018. 北京平原区南部PGZ01孔第四纪地层划分及其环境意义. 古地理学报, 20(2): 337-348. [Zhao Y,Wang Q,Li R J,Wei B,Xu J X,Sun Y H,Zhang X L,Wang C J,Zhou Y X,You S N,Lü J B.2018. Quarter-nary stratigraphic division and its environmental significance of Borehole PGZ01 in southern Beijing plain area. Journal of Palaeogeography(Chinese Edition), 20(2): 337-348] [32] 赵勇,李瑞杰,魏波,王纯君,孙永华,方同明. 2019. 北京大兴凸起南部PGZ05钻孔剖面第四纪磁性地层学. 现代地质, 33(1): 56-62. [Zhao Y,Li R J,Wei B,Wang C J,Sun Y H,Fang T M.2019. Magnetostratigraphy of Borehole PGZ05 in Southern Daxing Uplift,Beijing Plain. Geoscience, 33(1): 56-62] [33] Amorosi A,Bruno L,Campo B,Costagli B,Hong W,Piccotti V,Vaiani S C.2021. Deformation patern of upper Quaternary strata and their relation to active tectonics,Po Basin,Italy. Sedimentology, 68(1): 402-424. [34] ,Arnold J. H.Reesink, A J H,Ashworth P J. Smith G H S,Best J L,Parsons D R Amsler M L,Hardy R J,Lane S N,Nicolas A P,Orfeo O,Sandbach S D,Simpsen C J,Szuplny R N.2014. Scales and causes of heterogeneity in bars in a large multi-channel river: Río Paraná,Argentina. Sedimentology, 61(4): 1055-1085. [35] Breda A,Amorosi A,Rossi V,Fusco F.2016. Late-glacial to Holocene depositional architecture of the Ombrone palaeovalley system(Southern Tuscany,Italy): sea-level,climate and local control in valley-fill variability. Sedimentology, 63: 1124-1148. [36] Gugliotta M,Saito Y,Eguyen van L,Ta T K O,Tamura T.2019. Sediment distribution and depositional processes along the fluvial to marine transition zone of the Mekong River delta,Vietnam. Sedimentology, 66(1): 146-164. [37] Mail A D.1996. The Geology of Fluvial Deposits. Berlin: Springer,1-504. [38] Parham P R,Riggs S R,Culver S J,Mallinson D J,Rink W J,Burdette K.2013. Quaternary coastal lithofacies,sequence development and stratigraphy in a passive margin setting,North Carolina and Virginia,USA. Sedimentology, 60: 503-547. [39] Singer B S.2014. A Quaternary geomagnetic instability time scale. Quaternary Geochronology, 21(1): 29-52. [40] Wang Z B,Yang S Y,Wang Q,Zhang Z X,Zhang X H,Lan X H,Li R H,Huang L.2014. Late Quaternary stratigraphic evolution on the outer shelf of the East China Sea. Continental Shelf Research, 90: 5-16. [41] Yao Z Q,Shi X F,Liu Q S,Liu Y G,Larrasoaña J C,Liu J X,Ge S L,Wang K S,Qiao S Q,Li X Y,Shi F D,Fang X S,Yu Y G,Yang G,Duan Z Q.2014. Paleomagnetic and astronomical dating of sediment core BH08 from the Bohai Sea,China: implications for glacial-interglacial sedimentation. Palaeogeography,Palaeoclimatology, Palaeoecology, 393: 90-101.