近20年来中国古河道研究进展

doi:10.11820/dlkxjz.2013.01.001

摘要/Abstract

摘要： 近20年来,我国在嫩江大安古河道、莱州湾南岸平原古河道、长江南京以下段古河道及古深槽、海底古河道等区域的研究,获得了大量研究成果,深化了理论认识,拓展了应用领域。这些新成果与新认识进一步表明,中国各外流大河均有末次盛冰期埋藏古河道,该期古河流深切于末次冰期间冰阶的陆地及浅海大陆架,形成切割谷和谷底部的深槽,谷内堆积了末次盛冰期和早全新世的河流相滞留物质和粗颗粒物质,上部被中全新世海相、海陆交互相或陆相细粒物质覆盖,构成了埋深约20~50 m的浅埋古河道带。古河道中蕴藏着比较丰富的地下淡水,是洪冲积平原及浅海陆架地区的重要水源。

关键词: 地下淡水, 末次盛冰期, 浅埋古河道, 研究进展

Abstract: The last 20 years have seen new progresses in palaeochannel studies in China, including the investigations on palaeochannels in Nenjiang Daan, palaeochannels in the plain south of Laizhou bay, and palaeochannels, deep ancient grooves and submarine palaeochannels in the Yangtze river downstream of Nanjing, and so on. As a result, a large number of achievements have been accomplished, and new theories proposed; the research achievements have found new applications as well. The new knowledge and new theories indicate that buried palaeochannels exist in all of large outflowing rivers in China since the LGM(Last Glacial Maximum). The palaeochannel runs deep into the stadial terrestrial and the sea bed of the continental shelf from the Last Glacial Epoch, forming a cutting valley with deep grooves at the bottom, stacked with fluvial carryover and coarse particulate material from the LGM and early Holocene. The upper part of the valley is covered with marine, paralic, and continental fine-grained material from the Holocene, which frames the shallow-buried palaeochannel with 20 m to 50 m depth. Palaeochannels are rich in underground water, and an important water source for the areas of alluvial plain and shallow continental shelf.

Key words: shallow-buried palaeochannel, study progress, the Last Gracial Maximum(LGM), underground water

赵艳霞, 徐全洪, 刘芳圆, 秦彦杰, 吴忱, 陈利江, 崔俊辉. 近20年来中国古河道研究进展[J]. 地理科学进展, 2013, 32(1): 3-19.

ZHAO Yanxia, XU Quanhong, LIU Fangyuan, QIN Yanjie, WU Chen, CHEN Lijiang, CUI Junhui. Progresses of palaeochannel studies in China in the past 20 years[J]. PROGRESS IN GEOGRAPHY, 2013, 32(1): 3-19.

参考文献

[1] Bao C W.1995.Buried ancient channels and deltasin the Zhujiang River mouth shelf area.Marine Geology&Quaternary Geology,15(2):25-34.[鲍才旺.1995.珠江口陆架区埋藏古河道与古三角洲.海洋地质与第四纪地质,15 (2):25-34.]

[2] Cao G J,Wang J,Qu G X.2006a.An overview of the research on channel evolution in the Yangtze River mouth region since the Last Glacial Maximum.Advances in Earth Science,21(10):1039-1045.[曹光杰,王建,屈贵贤. 2006a.末次盛冰期以来长江河口段河道演变研究综述.地球科学进展,21(10):1039-1045.]

[3] Cao G J,Wang J,Xiong W Y,et al.2006b.Sedimentary characteristics of the Yangtze River's paleovalley in Nanjing since the Last Glacial Maximum.Marine Geology&Quaternary Geology,26(1):23-28.[曹光杰,王建,熊万英,等.2006b.长江南京段末次盛冰期以来的古河谷沉积.海洋地质与第四纪地质,26(1):23-28.]

[4] Cao G J,Li Y Y.2009a.Characteristics of Nanjing paleovalley section of the Yangtze River during the Last Glacial Maximum.Marine Geology&Quaternary Geology,29 (3):39-42.[曹光杰,李彦彦.2009a.末次盛冰期长江南京段古河槽特征.海洋地质与第四纪地质,29(3): 39-42.]

[5] Cao G J,Wang J,Zhang X Q,et al.2009b.Characteristics and run off volume of the Yangtze River paleovalley at Nanjing reach in the Last Glacial Maximum.Geographica Sinica,64(3):331-338.[曹光杰,王建,张学勤,等.2009b. 末次盛冰期长江南京段河槽特征及古流量.地理学报, 64(3):331-338.]

[6] Cao G J,Zhang Y L,Li Y Y.2011.The paleovalley in Xiaguan-Qixia Mountain of Nanjing reach of the Yangtze River during the Last Glacial Maximum.Journal of Mountain Science,29(2):183-187.[曹光杰,张玉兰,李彦彦.2011.末次盛冰期长江南京下关—栖霞山段的古河槽.山地学报,29(2):183-187.]

[7] Chen J P,Zhang A F,Cui T C.2010.Analysison planting the landscape for the bank of the ancient cannalin Zhaoqing. Advancesin Ornamental Horti culture of China//Chinese Society for Horticultural Science.Beijing:China,Forestry Publishing House:551-554.[陈锦屏,张爱芳,崔铁成.2010.浅谈肇庆古河道植物造景规划设计//中国园艺学会.北京:中国林业出版社:551-554.]

[8] Chen S T,Zhang C,Li Q R.2004.Methods and effects of the application along the layer attribute analysis techniques to identify the ancient river//Geological Society of China.The 8th of palaeogeography and sedimentology conference abstracts sets.Daqing,China:127-128.[陈守田, 张财,李清仁.2004.应用沿层属性分析技术识别古河道的方法及效果//中国地质学会.第八届古地理学与沉积学学术会议论文摘要集.大庆:127-128.]

[9] Chen Z X,Cao X Q,Huang H Y,et al.2009.Relationship between river cross section character sand change of ancient geography of offshorein Qingdao Bay.Acta Sedimentologica Sinica,27(1):109-110.[陈正新,曹雪晴,黄海燕,等.2009.青岛近海古河道断面特征与古地理变迁关系研究.沉积学报,27(1):109-110.]

[10] Dai R L,Zhu J R,Cao H B.1990.Evaluation of tthe lique faction ancient stream channel of the foundation soil of the Wu-song river.Shanghai Geology,11(1):32-44.[戴荣良,朱金荣,曹惠宾.1990.吴淞江古河道地基土液化的评价.上海地质,11(1):32-44.]

[11] Deng J M,Qiu D Y,Shen X S.2010.The application of high-density resistivity prospectingin engineering investigation in Suzhou.Earthquake Research in Shanxi,(3): 27-30.[邓建梅,邱道友,沈晓松.2010.高密度电法测试在苏州地区工程勘察中的应用.山西地震,(3):27-30.]

[12] Duan Q B,Zhou K S.1991.Realation of the river near Chang'an city changes and ancient cultural distribution//Zhou K S.Environmental Archaeology Series.Beijing,China:Science Press:47-55.[段清波,周昆叔,1991.长安附近河道变迁与古文化分布//周昆叔.环境考古研究第一辑.北京:科学出版社:47-55.]

[13] Fan F X,Lin M H,Jiang R H,et al.1999.The submarine buried paleo-delta in the east outer continental shelf of Hainan Island.Marine Sciences,23(6):55-57.[范奉鑫,林美华,江荣华,等.1999.海南岛东部外陆架水下埋藏古三角洲.海洋科学,23(6):55-57.]

[14] Fang G X,Yang J C,Yang Y X.2003.A effect discussionof transient electromagnetic sounding techniquein paleochannel-type sandstone-hosted uranium deposit.Journal of East China Geological Institute,26(4):361-363. [方根显,杨建春,杨亚新.2003.瞬变电磁法在古河道型砂岩铀矿找矿中的应用.华东地质学院学报,26(4): 361-363.]

[15] Feng M Y.1999.Analysis on metallogenic conditions of paleochannel sandstone type uranium deposits in kelulun region.Uranium Geology,15(4):198-203.[冯明月. 1999.克鲁伦河盆地及其邻区古河道型砂岩铀矿成矿条件分析.铀矿地质,15(4):198-203.]

[16] Fu X J,Liu K Y,Li G M.2008.Symmetric quadrupole resistivity sounding curves with the electrical characteristics of the ancient river with Hejian.Ground Water,30(5): 107.[付新建,刘克宇,李改梅.2008.对称四极电阻率测深曲线在古河道带及河间带的电性特征.地下水,30 (5):107.]

[17] Fu X L,Li R Q.1998.A preliminary study on the paleochannel of the Huaihe River in the Huainan area.Journal of

[18] Beijing Normal University:Natural Science,34(2): 276-279.[傅先兰,李容全,1998.淮南地区淮河故道的初步研究.北京师范大学学报:自然科学版,34(2): 276-279.]

[19] Gao D M,Chen Z R,Lu Q R.1998.Engineering geological feature study of paleochannel drowned-valley facies stratain the Shanghai Land Area.Shanghai Geology,19(4): 11-21.[高大铭,陈振荣,吕全荣.1998.上海陆域地区古河道溺谷相沉积层工程地质特征研究.上海地质,19 (4):11-21.]

[20] Guo H D,Liu H,Wang X Y,et al.2000,Spaceborne imaging radar and paleoenvironment the alashan plateau of forested ancient water system to detect.Science China:Series D,30(1):88-96.[郭华东,刘浩,王心源,等.2000.航天成像雷达对阿拉善高原次地表古水系探测与古环境分析.中国科学:D辑,30(1):88-96.]

[21] Han G R,Xu S S,Xin C Y.1998.Geochemical characteristics of the sediment in buried paleoriver channel area in the Huanghai Sea and Bohai Sea//Institute of China Oceanography.Bulletin of Marine Science.Beijing,China:Science Press:79-87.[韩桂荣,徐孝诗,辛春英.1998.黄海、渤海埋藏古河道区沉积物的地球化学特征//中国海洋研究所.海洋科学集刊.北京:科学出版社:79-87.]

[22] Han M,Li D G,Zhao M H,et al.1999.The study of the surface emerging ancient channels on the south coast plain of laizhou bay.Scientia Geographica Sinica,14(5): 451-456.[韩美,李道高,赵明华,等.1999.莱州湾南岸平原地面古河道研究.地理科学,14(5):451-456.]

[23] Han M,Zhao M H,Li D G,et al.1999.Study on the ancient channels and the relationship between the ancient channels and the sea(salt)water intrusion of the south coastal plain of laizhou bay.Journal of Natural Disasters,8(2): 73-80.[韩美,赵明华,李道高,等,1999.莱州湾南岸平原古河道及其与海(咸)水入侵关系研究.自然灾害学报,8(2):73-80.]

[24] Hao D Y,Liu G B,Yang Z L,et al.1992.The high-effective development mode of sandy wasteland farming at Hebei Longhua Town palaeochannel.Erritory&Natural Resources Stuty,1992(1):30-32.[郝德有,刘贵波,杨宗利,等.1992.河北省龙华镇古河道带沙荒地种植业高效益规模开发模式.国土与自然资源研究,(1):30-32.]

[25] He Q M.2002.Lanzhou east basin in the paleochannel change research.Lanzhou Institute of Education,2002(4): 22-28.[何启明.2002.兰州东盆地黄河古河道变迁研究.兰州教育学院学报,(4):22-28.]

[26] Hu G Y.2010.The paleoenvironmental before the Bohai Bay holocene transgression[D].Qingdao,China:Ocean University of China.[胡广元.2010.渤海湾全新世海侵前的古环境[D].青岛:中国海洋大学.]

[27] Hu J X,Li Z J,Zhang Y S.2007.Multi-attribute recognition technology in a thin layer of sand bodies of the ancient river//Chinese Geophysical Society.Annual Meeting Proceedings of the twenty-third of the Chinese Geophysical Society.Qingdao:China Ocean University Press: 138.[胡金祥,李宗杰,张永升.2007.多属性识别技术在古河道薄层砂体中的应用//中国地球物理学会,中国地球物理学会第二十三届年会论文集.青岛:中国海洋大学出版社:138.]

[28] Institute of Remote Sensing Applications,Chinese Academy of Sciences.1988.Remote sensing research of waters dynamic evolution at Huang-Huai-Hai Plain.Beijing:Science Press.[中国科学院遥感应用研究所.1988.黄淮海平原水域动态演变遥感研究.北京:科学出版社.]

[29] Jiang H,Wang Z C,Wang H,et al.2011.Recognizing palae-channels in Halaha tang area,North tarim by seismicse dimentology.Journal of Central South University:Science and Technology,42(12):135-142.[姜华,汪泽成, 王华,等.2011.地震沉积学在塔北哈拉哈塘地区古河道识别中的应用.中南大学学报:自然科学版,42(12): 135-142.]

[30] Jiang R F,Tao Y S,Zhang Q G.1995.Study on the availabilily of the micronutrient applicationin fine aandy aoilsin Heilonggang district.Acta Agriculturae Universitatis Pekinensis,21(S2):81-83.[江荣风,陶益寿,张起刚. 1995.黑龙港流域古河道细质沙土微肥有效性的研究. 北京农业大学学报,21(S2):81-83.]

[31] Jin Y N,Ji K Q,Qiu S P,et al.2004.Electricalproperty of quaternary ancient water course of Yinping and Huachong area,Jiangsu Province.Hydrogeology and Engineering Geology,31(3):99-101.[金永念,季克其,仇慎平,等. 2004.江苏阴平、华冲地区第四纪古河道电性特征研究.水文地质工程地质,31(3):99-101.]

[32] Kou Y Q,Du D L.1994.Sedimentary features of shallow ancient river channels on the northern shelf of the South China Sea.Acta Geologica Sinica,78(3):268-277.[寇养琦,杜德莉.1994.南海北部陆架第四纪古河道的沉积特征.地质学报,78(3):268-277.]

[33] Lei Q.1991.Governance sandy waste sandy raise three benefits.Hebei Agricultural Ecology,(2):21-26.[雷勤. 1991.治理沙荒沙地提高三大效益.河北农业生态, (2):21-26.]

[34] Li C X,Fan D D,Yang S Y,et al.2008.Characteristics and formation of the late quaternary in cised-valleys equencesinestuary and delta areas in China.Journal of Palaeogeography,10(1):87-97.[李从先,范代读,杨守业,等. 2008.中国河口三角洲地区晚第四纪下切河谷层序特征和形成.古地理学报,10(1):87-97.]

[35] Li C X,Zhang G J.1995.A sea-running Changjiang River during the Last Glaciation?Geographica Sinica,50(5): 459-463.[李从先,张桂甲.1995.末次冰期时存在入海的长江吗？地理学报,50(5):459-463.]

[36] Li D G,Han M,Zhao M H,et al.1999.A study of the shallow-buried paleochannel zones and their relations with-Sea(salt)-water intrusion on the south coast plain of Laizhou bay.Acta Oceanologica Sinica,21(6):64-71.[李道高,韩美,赵明华,等.1999.渤海莱州湾南岸平原浅埋古河道带及其与海(咸)水入侵关系研究.海洋学报,21 (6):64-71.]

[37] Li D G,Zhao M H,Han M,et al.2000.A study of the shallowly-buried paleochannel zones in the south coast plain of the Laizhou bay.Marine Geology&Quaternary Geology,20(1):23-29.[李道高,赵明华,韩美,等.2000.莱州湾南岸平原浅埋古河道带研究.海洋地质与第四纪地质,20(1):23-29.]

[38] Li J F.1991.The discover of the ancient river channel in Loulan and the estimate of wind erosion rate of wind erosion landform.Geographical Research,10(1):86-94.[李江风.1991.楼兰古河道的发现和风蚀地貌吹蚀速率的测算.地理研究,10(1):86-94.]

[39] Li F,Yu J J,Jiang X H,et al.1991.Study on buried Paleo-channel system in the south Yellow Sea.Oceanologia Et Limnologia Sinica,22(6):501-508.[李凡,于建军,姜秀珩,等.1991.南黄海埋藏古河系研究.海洋与湖沼,22(6):501-508.]

[40] Li F,Zhang X R,Li Y Z,et al.1998a.Buried paleo delta in the south Yellow Sea.Geographica Sinica,53(3): 238-244.[李凡,张秀荣,李永植,等.1998a.南黄海埋藏古三角洲.地理学报,53(3):238-244.]

[41] Li F,Zhang X R,Tang B Y.1998b.Atlas of Yellow Sea Buried Paleochannels and Ceological Hazards.Jinan,China:Jinan press.[李凡,张秀荣,唐宝钰.1998b.黄海埋藏古河道及灾害地质图集.济南:济南出版社.]

[42] Li G X,Liu Y,Yang Z G,et al.2005.The Yangtze River paleochannel at East China Sea shelf plain during the Last Glacial Period.Science in China:Ser.D,35(3): 284-289.[李广雪,刘勇,杨子赓,等.2005.末次冰期东海陆架平原上的长江古河道.中国科学:D辑,35(3): 284-289.]

[43] Li H C.1991.Buried water-rich palaeochannel exploration using integrated geophysical survey.Geology and Prospecting,(7):43-47.[李焕春.1991.利用综合物探方法寻找隐伏的富水古河道.地质与勘探,(7):43-47.]

[44] Li J H,2005.Analysis on percolation through ancient channel located in left bank of dam of Hengquan Reservoir.Shanxi Hydrotechnics,(4):11-12.[李江海.2005.横泉水库左岸古河道绕坝渗漏分析.山西水利科技,(4): 11-12.]

[45] Li M,Qiu C T,Guan S B.2009.Application test of CSAMT method to the exploration of paleo-channel sandstone type uranium deposit in Inner Mongolia.Uranium Geology,25(3):173-178.[李茂,丘崇涛,管少斌.2009.CSAMT法在内蒙古某古河道砂岩型铀矿勘查中的试验应用.铀矿地质,25(3):173-178.]

[46] Li Q R,Chen S T,Zhang C.2006.Identified approach of palaeochannel sand body in Haila'er basin.Oil Geophysical

[47] Prospecting,41(4):60-62.[李清仁,陈守田,张财. 2006.海拉尔盆地的古河道砂体识别方法.石油地球物理勘探,41(4):60-62.]

[48] Li X J.2006.Research on the types and exploitation models of saline soil in Da'an Ancient Riverway.Chinese Journal of Eco-Agriculture,14(3):111-113.[李秀军.2006. 大安古河道盐碱土类型与开发利用模式研究.中国生态农业学报,14(3):111-113.]

[49] Li X J,Sun G Y.2002.Dynamic model of agricultural system exploitation in Daan ancient river couse.System Sciemcesand Comprehensive Studies in Agriculture,18(1): 30-34.[李秀军,孙广友.2002.大安古河道农业系统动力学模型.农业系统科学与综合研究,18(1):30-34.]

[50] Lin C M,Li G Y,Zhuo H C,et al.2005.Sedimentary facies of incised valley fillings of the Late Quaternaryin Hangzhou Bay area and shallow biogenic gas exploration.Journal of Palaeogeography,7(1):12-24.[林春明,李广月,卓弘春,等.2005.杭洲湾地区晚第四纪下切河谷充填物沉积相与浅层生物气勘探.古地理学报,7(1): 12-24.]

[51] Liu A C,LüW Y,Cai F.2005.A buried meandering river of late quaternary off shantou city Guangdong province.Oceanologia Et Limnologia Sinica,36(2):104-110.[刘阿成,吕文英,蔡峰.2005.广东汕头南部近海晚第四纪埋藏古河曲的研究.海洋与湖沼,36(2):104-110.]

[52] Liu E F,Zhang Z L,Shen J,et al.2003.Sedimentary characteristics of Weihe palaeochannel sincelate pleistocene and their control to modern salt-water intrusion.Geological Journal of China Universities,9(1):47-53.[刘恩峰, 张祖陆,沈吉,等.2003.晚更新世以来潍河古河道沉积及其对现代咸水入侵的控制.高校地质学报,9(1): 47-53.]

[53] Liu J F,Chen J,Lei S X,et al.2009.Preliminary dating results for Qinhuai palaeochannel sediments in Nanjing city.Quaternary Sciences,29(4):837-844.[刘进峰,陈杰,雷生学,等.2009.南京市区埋藏古河道沉积物的年代.第四纪研究,29(4):837-844.]

[54] Liu K,Zhuang Z Y,Liu D Y,et al.2009a.Study of the buried ancient channels in the continental shelf area out of the mouth of the Changjiang River in China.Acta Oceanologica Sinica,31(5):80-88.[刘奎,庄振业,刘东雁,等. 2009a.长江口外陆架区埋藏古河道研究.海洋学报,31 (5):80-88.]

[55] Liu K,Zhuang Z Y,Liu D Y,et al.2009b.Pattern discrimination and characteristic analysis of the buried ancient channels in the inner continental shelf out of Yangtze River.Transactions of Oceanology and Limnology,2009 (1):79-87.[刘奎,庄振业,刘东雁,等.2009b.长江口外内陆架埋藏古河谷的河型判别方法探讨.海洋湖沼通报,(1):79-87.]

[56] Liu K,Zhuang Z Y,Liu D Y,et al.2010.Hydrology environment characteristics of buried ancient channels near Zhoushan islands and Yangtze River estuary.Journal of Jilin University:Earth Science Edition,40(1):140-147. [刘奎,庄振业,刘东雁,等.2010.舟山群岛和长江口邻近海域埋藏古河道水文环境特征.吉林大学学报:地球科学版,40(1):140-147.]

[57] Liu L W,Hao X G,Zhao W,et al.2006.Application of multi-attribute analysis to the identification of river palaeochannel in the thin interbeded reservoir.Journal of Daqing Petroleum Institute,30(4):4-6.[刘丽薇,郝兴国,赵伟,等.2006.多属性分析技术在薄互层条件下识别古河道的应用.大庆石油学院学报,30(4):4-6.]

[58] Liu Z C,Qin Y C,Jin S.2008.Study in treatment of Lower Yellow River Channel and its beach area's problem.Progressin Geography,27(2):32-38.[刘兆存,秦耀辰,金生.2008.黄河下游河道治理及滩区问题研究.地理科学进展,27(2):32-38.]

[59] Liu Z X,Berne S.2000.Paleochannels and paleodeltas in the continental shelf of the East China Sea.Marine Geology &Quaternary Geology,20(1):9-14.[刘振夏,Berne S. 2000.东海陆架的古河道和古三角洲.海洋地质与第四纪地质,20(1):9-14.]

[60] Luo J M,Yang F.2008.Micro scale feature of sodic saline soil and salt accumulation mechanism in surface layer:taking alkaline floodplain in Da'an County of Jilin province as an example.Journal of Soiland Water Conservation, 22(2):88-92.[罗金明,杨帆,邓伟,等.2008.苏打盐渍土的微域特征及土壤表层积盐机理探讨:以吉林省大安地区嫩江古河道盐滩地为例.水土保持学报,22(2): 88-92.]

[61] Luo X Zh,Liu N Y.1997.Da'an Palaeochannel area lakes and wetlands,the ecological environment and sustainable development of agriculture.Areal Research and Development,16(2):22-24.[罗新正,刘宁豫.1997.大安古河道区湖泊湿地的生态环境与农业可持续发展.地域研究与开发,16(2):22-24.]

[62] Luo X Z,Sun G Y.2007.Desalting experiment of intensely salt-affected soil by planting rice in the Da'an paleochannel of the Songnen plain.Chinese Journal of Soil Science,38(1):72-76.[罗新正,孙广友.2007.松嫩平原大安古河道强度盐渍土种稻脱盐试验.土壤通报,38(1): 72-76.]

[63] Luo X Z,Yi F K,Sun G Y.2000.Characteristics of alkaline lake wetland in Songnen plain and discussion about its agricultural development:taking Yaopao Lake of Da'an palaeochannel area for example.Scientia Geographica Sinica,20(5):483-486.[罗新正,易富科,孙广友.2000. 松嫩平原弱碱性湖泡湿地特征及其农业开发的探讨: 以大安古河道区腰泡为例.地理科学,20(5):483-486.]

[64] Luo X Z,Zhu T,Sun G Y.2003a.Wetland restoration and reconstruction in Da'an Paleochannel of Songnen Plain.Acta Ecologica Sinica,23(2):244-250.[罗新正,朱坦, 孙广友.2003a.松嫩平原大安古河道湿地的恢复与重建.生态学报,23(2):244-250.]

[65] Luo X Z,Zhu T,Sun G Y,et al.2003b.Demonstrating feasibility of geologic-landform environment for synthetically-developing ecologic engineerings in Da'an palaeochannels.Scientia Geographica Sinica,26(3):348-353. [罗新正,朱坦,孙广友,等.2003b.大安古河道综合开发生态工程地质地貌环境可行性论证.地理科学,26 (3):348-353.]

[66] Lv J B.2000.1:50000 regional geology and resources envi-ronment through field of the sourth of Beijing deep coverage area acceptance survey.Regional Geology of China,19(4):112.[吕金波.2000.北京城南深覆盖区1:5万区域地质与资源环境调查通过野外验收.中国区域地质,19(4):112.]

[67] Lv X,Chen L,Han F,et al.2011.Using paleochannel to building plain reservoirs at Laiwu Muwen-river.China Water Transport,11(8):188-189.[吕霞,陈蕾,韩锋,等.2011. 莱芜市牟汶河利用古河道兴建平原水库工程.中国水运,11(8):188-189.]

[68] Ma J P.1994.Formation and evolutionof Da'an palaeochannels at Nenjiang River right bank downstream.Scientia

[69] Geographica Sinica,14(2):194-196.[马建平.1994.嫩江下游右岸大安古河道的形成与演化.地理科学,14 (2):194-196.]

[70] Ma J P,Sun G Y,Xia Y M.2007.The formation period of Nenjiang downstream Da'an palaeochannel and depositional environment reconstruction//Sun G Y.2000.The Agricultural Engineering Research of Songnen Plain palaeochannel.Changchun,China:Jilin science and Technology Press:135-141.[马建平,孙广友,夏玉梅.2007.嫩江下游大安古河道的形成时代与沉积环境重建//孙广友.松嫩平原古河道农业工程研究.长春:吉林科学技术出版社:135-141.]

[71] Ma S Z,Liang K,Chen T H.2009.Guangxi Qinzhou Bay shallow sedimentary characteristics of buried ancient river//Chinese Ocean Engineering Society.Chinese Ocean Engineering Society Symposium Proceedings of the 14th China marine(offshore)engineering.Beijing:Ocean Press:1225-1229.[马胜中,梁开,陈太浩.2009. 广西钦州湾浅层埋藏古河道沉积特征//中国海洋工程学会.第十四届中国海洋(岸)工程学术讨论会论文集. 北京:海洋出版社:1225-1229.]

[72] Ma X,Zhou X Y.2011.Preservation of riverway landscape in historic and cultural city:A case of south inner Qinhuai River,Nanjing.Huazhong Architecture,29(4):147-149. [马晓,周学鹰.2011.历史文化名城中古河道景观的认识与保护:以南京内秦淮河城南段为例.华中建筑,29 (4):147-149.]

[73] Meng Q H,Han M,Zhao M H,et al.1999.A preliminary study of the Mihe River alluvial diluvial fan and the palaeochannels.Journal Of Shandong Normal University:Natural Science,14(1):47-51.[孟庆海,韩美,赵明华, 等.1999.弥河冲洪积扇和古河道初步研究.山东师范大学学报:自然科学版,14(1):47-51.]

[74] Nie X H,Liu E F,Zhang Z L.2001.Shallowly buried ancient channels and quaternary strata division in the lower reaches of the Weihe River.Marine Geology&Quaternary Geology,21(4):89-94.[聂晓红,刘恩峰,张祖陆. 2001.潍河下游地区浅埋古河道沉积与第四系地层划分.海洋地质与第四纪地质,21(4):89-94.]

[75] Peng X M.2003.Palaeochannel of the capital:Chang river.Beijing Archives,(3):48-49.[彭晓梅.2003.京城古河道:长河.北京档案,(3):48-49.]