Sedimentary environment evolution of the paleochannel in the middle reaches of Hutuo River since 150, 000 years and its response of climate change
-
摘要:
古河道记载了地质历史时期区域水系结构和沉积环境的演变信息,对复原古环境、水系变迁规律等具有重要理论意义。依托滹沱河冲洪积扇扇中古河道带上的一个第四纪钻孔(L2),基于详细的岩性特征、粒度参数和光释光年龄数据,文章深入分析了古河道发育的期次和时段,探讨了滹沱河中游古河道带150 ka以来的沉积环境演变过程及其对气候变化的响应。结果表明:研究区150 ka以来的沉积环境演化主要表现为三期古河道发育期与两期河流稳定期的交替,与深海氧同位素阶段及其指示的气候冷暖变化有很好的对应关系。其中三期古河道发育期分别对应于深海氧同位素第2、4、6阶段及其指示的气候冷期,两期河流稳定期对应于深海氧同位素第3、5阶段及其指示的气候暖期。第三期古河道(118~151 ka)是由距今150 ka的共和运动引起的构造抬升与倒数第二次冰期冷干气候的共同作用形成;第二期古河道(36~76 ka)是区域间歇性构造抬升与气候变化共同作用的结果;而第一期古河道(5~26 ka)则是末次盛冰期气候变化的产物。
Abstract:Palaeochannel records the evolution information of regional drainage system structure and sedimentary environment in geological history, which is of great theoretical significance to the restoration of palaeoenvironment and the evolution law of drainage system. Based on a Quaternary borehole (L2) in the paleochannel of the alluvial and diluvial fan of Hutuo River, detailed lithological characteristics, grain size parameters and optical ages, the development periods and sedimentary environment evolution of the paleochannel in the middle of Hutuo River since 150, 000 years and its response of climate change was discussed. The results show that the sedimentary environment evolution of the study area is mainly composed of three paleochannel development periods and two river stabilization periods since 150, 000 years. It has a good correspondence with the deep-sea oxygen isotope stage and the climate change indicated. The three periods of paleochannel development correspond to the second, fourth and sixth stages of the deep-sea oxygen isotopes, and the cold climate respectively. Two river stabilization periods corresponds to the third and fifth stages of the deep-sea oxygen isotopes, and the warm climate respectively. The third paleochannel (about 151~118 ka) was formed by the combination of tectonic uplift caused by the republican movement 150 thousand years ago and the cold-dry climate during the penultimate glaciation. The second palaeochannel (about 76~36 ka) is the result of intermittent regional tectonic uplift and climate change. And the first palaeochannel (about 26~5 ka) was the result of climate change during the last glacial maximum.
-
-
图 4 L2孔沉积环境演变综合图(岩性图例同图 2)
Figure 4.
表 1 L2孔沉积物光释光年龄
Table 1. Luminescence age of the sediments in the borehole L2
-
Chen Zhongyuan, Yan Qinshang. 1982. The structural features of recent alluvial sedimentation of the Hutuo River on plain reach, Hebei Province[J]. Scientia Geographica Sinica, (3): 210-220 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKX198203002.htm
Cheng Shaoping, Ran Yongkang. 1981. Hutuo River terraces in Taihang canyon section and Quaternary tectonic movement[J]. Seismology and Geology, (1): 29-39 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZDZ198101005.htm
Cui Zhijiu, Chen Yixin, Zhang Wei, Zhou Shangzhe, Zhou Liping, Zhang Mei, Li Chuanchuan. 2011. Research history, glacial chronology and origins of Quaternary glaciations in China[J]. Quaternary Sciences, (5): 749-764 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ201105001.htm
Fan Shuxian, Liu Haikun, Xu Jianming, Zheng Hongrui, Zhao Hua, Bi Zhiwei, Yang Zhenjing, Lin Fang, Zhang Jing. 2009. Palaeovegetation and environmental evolution in Hengshui district of Hebei Province since 3.50 Ma BP[J]. Geoscience, 23(1): 75-81 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200901011.htm
Gao Zhanwu, Wu Hao, Li Guangtao, Cheng Li. 2014. Late Quaternery activity of the central-north segment of Taihang Mountain piedment fault zone[J]. Technology for Earthquake Disaster Prevention, 9(2): 159-170 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZZFY201402001.htm
He Naihua, Zhu Xuanqing, Liu Yixu. 1989. The paleochannel sediments and groundwater of the Hutuo River[J]. Journal of the Hebei Academy of Sciences, (1): 63-69 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-HBKX198901008.htm
Huang Huiyu. 1992. Composition and sedimentary environment of recent sediments of the Hutuo River on plain reach[J]. Journal of Tongji University, (4): 467-473 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-tjdz199204023.htm
Li Jijun, Fang Xiaomin, Ma Haizhou, Zhu Junjie, Pan Baotian, Chen Huailu. 1996. Geomorphological evolution of the upper Yellow River in the Late Cenozoic and the uplift of the Qinghai-Tibet Plateau[J]. Science in China(Series D), (4): 316-322 (in Chinese). http://www.cnki.com.cn/Article/CJFD1996-JDXG199604004.htm
Li Yusong, Chen Jianqiang, Zhao Shuo, Wang Haiying, Li Xin. 2011. Sporopollen assemblages in Tangshan area since Late Pleistocene with a correlation to those in adjacent areas[J]. Acta Geoscientica Sinica, 32(2): 178-188 (in Chinese with English abstract). http://www.researchgate.net/publication/303198406_Sporopollen_assemblages_in_tangshan_area_since_late_pleistocene_with_a_correlation_to_those_in_adjacent_areas
Liu Dongsheng, An Zhisheng, Sun Donghuai, Chen Mingyang. 1996. Preliminary comparison of the paleoclimate between the southern and northern hemispheres in recent 0.6 Ma[J]. Science in China(Series D), (2): 97-102 (in Chinese). http://www.cqvip.com/QK/60111X/19962/4001138884.html
Liu Jiaqi, Chen Tiemei, Nie Gaozhong, Song Chunyu, Guo Zhengtang, Li Kun, Gao Shijun, Qiao Yulou, Ma Zhibang. 1994. Datings and reconstruction of the high resolution time series in the Weinan loess section of the last 150, 000 years[J]. Quaternary Sciences, (3): 193-202 (in Chinese with English abstract). http://www.researchgate.net/publication/308048383_Dating_and_reconstruction_of_the_high_resolution_time_series_in_the_Weinan_loess_section_of_the_last_150_000_years
Liu Jiaqi, Ni Yunyan, Chu Guoqiang. 2001. Main palaeoclimatic events in the Quaternary[J]. Quaternary Sciences, (3): 239-248 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ200103005.htm
Liu Xingqi, Chi Zhenqing, Herzschuh Ulrike, Wang Yong, Ni Jian, Xu Qinghai. 2014. A MIS 3 charcoal and pollen record and quantitative precipitation inferences from the Jingerwa section of the Nihewan Basin, north-central China[J]. Journal of Paleolimnology, 51(2): 211-221. doi: 10.1007/s10933-013-9716-8
Liu Zhijie, Sun Yongjun. 2007. Uplift of the Qinghai-Tibet Plateau and formation, evolution of the Yellow River[J]. Geography and Geo-Information Science, (1): 79-82 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-DLGT200701018.htm
Tong Guobang, Zhang Junpai, Yan Fuhua, Mai Xueshun. 1991. Sporo-pollen sequence and division of climatic period in the eastern North China Plain since Late Pleistocene[J]. Seismology and Geology, (3): 259-268 (in Chinese with English abstract). http://www.researchgate.net/publication/294299345_Sporo-pollen_sequence_and_division_of_climatic_period_in_the_eastern_North_China_Plain_since_late_Pleistocene
Wang Pinxian, Min Qiubao, Bian Yunhua, Cheng Xinrong. 1981. Strata of Quaternary transgressions in east China: A preliminary study[J]. Acta Geologica Sinica, (1): 1-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE198101000.htm
Wang Qiang, Liu Lijun, Wang Weidong, Xu Haizhen, Sun Weiyi. 2004. The mechanism of Quaternary palaeoenvironmental change in Circum-Bohai Sea region and North China Plain[J]. Geological Survey and Research, (3): 129-138 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ200403001.htm
Wang Qiang, Zhang Yufa, Yuan Guibang, Zhang Wenqing. 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). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DSJJ200801010.htm
Wang Zhongbo, Zhang Jiangyong, Mei Xi, Chen Xiaohui, Zhao Li, Zhang Yong, Zhang Zhixun, Li Xuejie, Li Rihui, Lu Kai, Sun Rongtao, Yang Shouye. 2020. The stratigraphy and depositional environments of China's sea shelves since MIS5 74-128 ka[J]. Geology in China, 47(5): 1370-1394(in Chinese with English abstract).
Wu Bangyu, He Naihua, Shi Derong, Zhu Xuanqing, Huang Huiyu. 1983. Recent fluvial sedimentation of the Hutuo River, Hebei Province[J]. Journal of Tongji University, (2): 82-95 (in Chinese with English abstract).
Wu Chen, Zhu Xuanqing, He Naihua, Xu Qinghai, Yuan Wenying, Wang Zihui, Shi Derong, Zhao Mingxuan. 1991. Study on formation of paleochannels in North China Plain[J]. Science in China(Series B), (2): 188-197 (in Chinese with English abstract). http://qikan.cqvip.com/Qikan/Article/Detail?id=1005239304
Wu Chen, Xu Qinghai, Zhao Mingxuan. 1992. All major rivers in the world have buried paleochannels[J]. Geography and Territorial Researth, (2): 29-34 (in Chinese with English abstract).
Wu Chen, Ma Yonghong, Zhang Xiuqing. 1996. Palaeochannel and palaeodrainage patterns in the North China mountains[J]. Geographical Research, (3): 33-41 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLYJ603.004.htm
Wu Chen. 2001. Changes of river system and new tectonic movement in North China mountainous area[J]. North China Earthquake Sciences, (4): 1-6 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/hbdzkx200104001
Xiao Jingyi, Chen Jianqiang, Li Hui, Xu Zheping, Sun Gang, Niu Caixiang, Yang Guochen. 2008. Quantitative analysis of Quaternary sporopollen assemblages: A case study of hole HZ-S core in Handan, Hebei, China[J]. Geological Bulletin of China, (5): 599-604 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200805003.htm
Xiao Jingyi, Chen Jianqiang, Xu Zheping, Cao Guangchao, Zhao Qinglin, Gao Liwen. 2010. Characteristics of vegetation fluctuation as well as consequent impact on climate since Late Pleistocene in Handan Area, Hebei[J]. Acta Sedimentologica Sinica, 28(6): 1206-1212 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB201006020.htm
Xu Qinghai, Wu Chen, Yuan Wenying. 1988. Basic characteristics of natural environment evolution in Shijiazhuang Area at the end of Late Pleistocene[J]. Geography and Territorial Researth, (1): 51-55 (in Chinese with English abstract).
Yang Huifeng, Cao Wengeng, Zhi Chuanshun, Li Zeyan, Bao Xilin, Ren Yu, Liu Futian, Fan Cunliang, Wang Shufang, Wang Yabin. 2021. Evolution of groundwater level in the North China Plain in the past 40 years and suggestions on its overexploitation treatment[J]. Geology in China, 48(4): 1142-1155(in Chinese with English abstract).
Yao Tandong, Shi Yafeng, Qin Dahe, Jiao Keqin, Yang Zhihong, Tian Lide, Thompson L G, Mosley-Thompson E. 1997. Climate change records since the last interglacial period in the Guliya ice core[J]. Science in China(Series D), (5): 447-452 (in Chinese).
Yao Tandong, Xu Boqing, Pu Jianchen. 2001. Climatic changes on the orbit and suborbit time scales recorded by the Guliya ice core on the Qinghai-Tibet Plateau[J]. Science in China(Series D), (S1): 287-294 (in Chinese). http://www.cnki.com.cn/Article/CJFDTotal-JDXG2001S1042.htm
Zhang Lei, Zhang Xujiao, Wu Fadong, He Zexin, Tian Jun, Yu Hang, Wang Chunlin, Liu Jianghong. 2013. River terraces development and significance of neotectonic movement on the southern margin of Taihang Mountains since Late Pleistocene[J]. Geoscience, 27(4): 791-798 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ201304007.htm
Zhang Zhaoji, Luo Guozhong, Wang Zhao, Liu Chunhua, Li Yasong, Jiang Xianqiao. 2009. Study on sustainable utilization of groundwater in North China Plain[J]. Resources Science, 31(3): 355-360 (in Chinese with English abstract). http://www.oalib.com/paper/1703510
Zhao Hongmei, Liu Linjing, Zhao Hua, Bi Zhiwei, Wang Likang, Song Lei, Wang Chengmin, Yang Jingsong. 2016. Grain size character and sedimentary environment of Hutuo River paleochannel section[J]. Geoscience, (2): 485-492 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ201602027.htm
Zhao Hongmei, Liu Linjing, Zhao Hua, Bi Zhiwei, Wang Chengmin, Yang Jingsong, Wang Likang. 2019. High resolution stratigraphic sequence and sedimentary characteristics in Late Quaternary of Hutuo River paleochannel[J]. Journal of Stratigraphy, 43(4): 389-400 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DCXZ201904005.htm
Zhao Xitao, Zhu Dagang, Yan Fuhua, Wu Zhonghai, Ma Zhibang, Mai Xueshun. 2003. Climatic change and lake-level veriation of Nam Co, Xizang since the last interglacial stage[J]. Quaternary Sciences, (1): 41-52 (in Chinese with English abstract).
Zhao Yanxia, Xu Quanhong, Liu Fangyuan, Qin Yanjie, Wu Chen, Chen Lijiang, Cui Junhui. 2013. Progresses of palaeochannel studies in China in the past 20 years[J]. Progress in Geography, (1): 3-19 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLKJ201301002.htm
Zhao Yingshi. 1987. Palaeoclimate variability of the North China Plain for the last 120000 years[J]. Geographical Research, (4): 54-61 (in Chinese with English abstract).
Zheng Mianping, Yuan Heran, Zhao Xitao, Liu Xifang. 2006. The Quaternary pan-lake(overflow) period and paleoclimate on the Qinghai-Tibet Plateau[J]. Acta Geologica Sinica, (2): 169-180 (in Chinese with English abstract).
Zhu Xuanqing, He Naihua, Shi Derong, Wu Bangyu. 1985. Characteristics of sediment deposited in the lower reaches of the Hutuo River[J]. Journal of Sediment Research, (1): 22-31 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-NSYJ198501002.htm
Zhu Xuanqing, He Naihua. 1990. Reconstruction of stream morphology by the method of size analysis in Hutuo River[J]. Journal of the Hebei Academy of Sciences, (1): 17-29 (in Chinese with English abstract). http://d.wanfangdata.com.cn/periodical/QK000001213537
陈中原, 严钦尚. 1982. 滹沱河平原段现代沉积结构、构造特征[J]. 地理科学, (3): 210-220. https://www.cnki.com.cn/Article/CJFDTOTAL-DLKX198203002.htm
程绍平, 冉勇康. 1981. 滹沱河太行山山峡段河流阶地和第四纪构造运动[J]. 地震地质, (1): 29-39. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ198101005.htm
崔之久, 陈艺鑫, 张威, 周尚哲, 周力平, 张梅, 李川川. 2011. 中国第四纪冰期历史、特征及成因探讨[J]. 第四纪研究, (5): 749-764. doi: 10.3969/j.issn.1001-7410.2011.05.01
范淑贤, 刘海坤, 徐建明, 郑宏瑞, 赵华, 毕志伟, 杨振京, 林防, 张静. 2009. 3.50 Ma BP以来河北衡水地区古植被与环境演化[J]. 现代地质, 23(1): 75-81. doi: 10.3969/j.issn.1000-8527.2009.01.011
高战武, 吴昊, 李光涛, 程理. 2014. 太行山山前断裂带中北段晚第四纪活动性研究[J]. 震灾防御技术, 9(2): 159-170. doi: 10.3969/j.issn.1673-5722.2014.02.001
何乃华, 朱宣清, 刘益旭. 1989. 滹沱河古河道沉积和古河道地下水[J]. 河北省科学院学报, (1): 63-69. https://www.cnki.com.cn/Article/CJFDTOTAL-HBKX198901008.htm
黄惠玉. 1992. 滹沱河平原段现代沉积物的成分与沉积环境[J]. 同济大学学报(自然科学版), (4): 467-473. https://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ199204023.htm
李吉均, 方小敏, 马海洲, 朱俊杰, 潘保田, 陈怀录. 1996. 晚新生代黄河上游地貌演化与青藏高原隆起[J]. 中国科学(D辑: 地球科学), (4): 316-322. doi: 10.3321/j.issn:1006-9267.1996.04.005
李玉嵩, 陈建强, 赵硕, 王海英, 李欣. 2011. 唐山地区晚更新世以来的孢粉组合特征及其与邻区的对比[J]. 地球学报, 32(2): 178-188. doi: 10.3975/cagsb.2011.02.06
刘东生, 安芷生, 孙东怀, 陈明扬. 1996. 最近0.6 Ma南、北半球古气候对比初探[J]. 中国科学(D辑: 地球科学), (2): 97-102. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199602000.htm
刘嘉麒, 陈铁梅, 聂高众, 宋春郁, 郭正堂, 李坤, 高世君, 乔玉楼, 马志邦. 1994. 渭南黄土剖面的年龄测定及15万年来高分辨时间序列的建立[J]. 第四纪研究, (3): 193-202. doi: 10.3321/j.issn:1001-7410.1994.03.001
刘嘉麒, 倪云燕, 储国强. 2001. 第四纪的主要气候事件[J]. 第四纪研究, (3): 239-248. doi: 10.3321/j.issn:1001-7410.2001.03.006
刘志杰, 孙永军. 2007. 青藏高原隆升与黄河形成演化[J]. 地理与地理信息科学, (1): 79-82. https://www.cnki.com.cn/Article/CJFDTOTAL-DLGT200701018.htm
童国榜, 张俊牌, 严富华, 麦学舜. 1991. 华北平原东部地区晚更新世以来的孢粉序列与气候分期[J]. 地震地质, (3): 259-268. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDZ199103012.htm
汪品先, 闵秋宝, 卞云华, 成鑫荣. 1981. 我国东部第四纪海侵地层的初步研究[J]. 地质学报, (1): 1-13. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198101000.htm
王强, 刘立军, 王卫东, 徐海振, 孙维义. 2004. 环渤海地区及华北平原第四纪古环境变迁机制[J]. 地质调查与研究, (3): 129-138. doi: 10.3969/j.issn.1672-4135.2004.03.001
王强, 张玉发, 袁桂邦, 张文卿. 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
王中波, 张江勇, 梅西, 陈晓辉, 赵利, 张勇, 张志珣, 李学杰, 李日辉, 陆凯, 孙荣涛, 杨守业. 2020. 中国陆架海MIS5(74~128 ka)以来地层及其沉积环境[J]. 中国地质, 47(5): 1370-1394. http://geochina.cgs.gov.cn/geochina/ch/reader/view_abstract.aspx?file_no=20200507&flag=1
吴邦毓, 何乃华, 施德荣, 朱宣清, 黄惠玉. 1983. 滹沱河现代沉积相标志研究[J]. 同济大学学报, (2): 82-95. https://www.cnki.com.cn/Article/CJFDTOTAL-TJDZ198302007.htm
吴忱, 朱宣清, 何乃华, 许清海, 袁文英, 王子惠, 施德荣, 赵明轩. 1991. 华北平原古河道的形成研究[J]. 中国科学(B辑), (2): 188-197. https://www.cnki.com.cn/Article/CJFDTOTAL-JBXK199102010.htm
吴忱, 许清海, 赵明轩. 1992. 世界所有大河都有埋藏古河道[J]. 地理学与国土研究, (2): 29-34. https://www.cnki.com.cn/Article/CJFDTOTAL-DLGT199202006.htm
吴忱, 马永红, 张秀清. 1996. 华北山地的古河道与古水系[J]. 地理研究, (3): 33-41. https://www.cnki.com.cn/Article/CJFDTOTAL-DLYJ603.004.htm
吴忱. 2001. 华北山地的水系变迁与新构造运动[J]. 华北地震科学, (4): 1-6. doi: 10.3969/j.issn.1003-1375.2001.04.001
肖景义, 陈建强, 李辉, 许哲平, 孙刚, 牛彩香, 杨国臣. 2008. 河北邯郸HZ-S孔第四纪孢粉组合的定量分析[J]. 地质通报, (5): 599-604. doi: 10.3969/j.issn.1671-2552.2008.05.002
肖景义, 陈建强, 许哲平, 曹广超, 赵青林, 高丽文. 2010. 邯郸地区晚更新世以来植被波动特征及其对气候变化的响应[J]. 沉积学报, 28(6): 1206-1212. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201006020.htm
许清海, 吴忱, 袁文英. 1988. 晚更新世末期石家庄地区自然环境演变的基本特征[J]. 地理学与国土研究, (1): 51-55. https://www.cnki.com.cn/Article/CJFDTOTAL-DLGT198801010.htm
杨会峰, 曹文庚, 支传顺, 李泽岩, 包锡麟, 任宇, 柳富田, 范存良, 王树芳, 王亚斌. 2021. 近40年来华北平原地下水位演变研究及其超采治理建议[J]. 中国地质, 48(4): 1142-1155. http://geochina.cgs.gov.cn/geochina/ch/reader/view_abstract.aspx?file_no=20210411&flag=1
姚檀栋, 施雅风, 秦大河, 焦克勤, 杨志红, 田立德, Thompson L G, Mosley-Thompson E. 1997. 古里雅冰芯中末次间冰期以来气候变化记录研究[J]. 中国科学(D辑: 地球科学), (5): 447-452. doi: 10.3321/j.issn:1006-9267.1997.05.006
姚檀栋, 徐柏青, 蒲健辰. 2001. 青藏高原古里雅冰芯记录的轨道、亚轨道时间尺度的气候变化[J]. 中国科学(D辑: 地球科学), (S1): 287-294. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2001S1043.htm
张蕾, 张绪教, 武法东, 何泽新, 田珺, 于航, 王春林, 刘江红. 2013. 太行山南缘晚更新世以来河流阶地的发育及其新构造运动意义[J]. 现代地质, 27(4): 791-798. doi: 10.3969/j.issn.1000-8527.2013.04.005
张兆吉, 雒国中, 王昭, 刘春华, 李亚松, 姜先桥. 2009. 华北平原地下水资源可持续利用研究[J]. 资源科学, 31(3): 355-360. doi: 10.3321/j.issn:1007-7588.2009.03.001
赵红梅, 刘林敬, 赵华, 毕志伟, 王利康, 宋磊, 王成敏, 杨劲松. 2016. 滹沱河古河道剖面粒度参数特征及沉积环境[J]. 现代地质, (2): 485-492. doi: 10.3969/j.issn.1000-8527.2016.02.027
赵红梅, 刘林敬, 赵华, 毕志伟, 王成敏, 杨劲松, 王利康. 2019. 滹沱河古河道晚第四纪高分辨率地层层序及沉积特征[J]. 地层学杂志, 43(4): 389-400. https://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ201904005.htm
赵希涛, 朱大岗, 严富华, 吴中海, 马志邦, 麦学舜. 2003. 西藏纳木错末次间冰期以来的气候变迁与湖面变化[J]. 第四纪研究, (1): 41-52. doi: 10.3321/j.issn:1001-7410.2003.01.005
赵艳霞, 徐全洪, 刘芳圆, 秦彦杰, 吴忱, 陈利江, 崔俊辉. 2013. 近20年来中国古河道研究进展[J]. 地理科学进展, (1): 3-19. https://www.cnki.com.cn/Article/CJFDTOTAL-DLKJ201301002.htm
赵英时. 1987. 华北平原12万年以来的古气候变化[J]. 地理研究, (4): 54-61. https://www.cnki.com.cn/Article/CJFDTOTAL-DLYJ198704005.htm
郑绵平, 袁鹤然, 赵希涛, 刘喜方. 2006. 青藏高原第四纪泛湖期与古气候[J]. 地质学报, (2): 169-180. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200602000.htm
朱宣清, 何乃华, 施德荣, 吴邦毓. 1985. 滹沱河下游沉积泥沙的特征[J]. 泥沙研究, (1): 22-31. https://www.cnki.com.cn/Article/CJFDTOTAL-NSYJ198501002.htm
朱宣清, 何乃华. 1990. 运用粒度分析方法恢复河流地貌——以滹沱河为例[J]. 河北省科学院学报, (1): 17-29. https://www.cnki.com.cn/Article/CJFDTOTAL-HBKX199001003.htm
-