长江中游地区构造活动对河流地貌和人类活动的影响
|
摘要
论文主要研究长江中游地区第四纪的构造运动对该地区的河流地貌以及人类活动的影响。长江中游地区在全新世的构造活动较为简单,主要有挤压作用产生的隆起、褶皱以及掀斜作用,还有下沉作用等。一系列的构造运动形成了该地区的地貌形态:平原,盆地、丘陵等。其中洞庭平原、江汉平原,距离水源较近,土壤肥沃,地貌在全新世较为稳定,适宜人类居住,存在许多古人类遗址的遗存,随着构造运动的发展以及河流地貌的变迁,古人类遗址也发生着迁移,构造运动在一定程度上影响着先民生存地点的选择。
The study mainly studies the influence of Quaternary tectonic movements on the river landform and human activities in the middle reaches of the Yangtze River.The tectonic activities in the middle reaches of the Yangtze River during the Holocene are relatively simple, mainly due to the uplift, folds, tilting, and sinking effects. A series of tectonic movements formed the geomorphic forms of the region, mainly including plains, basins and hills. The Dongting plain and Jianghan Plain are close to the water source. The soil is fertile. The landform is more stable in the Holocene, and it is suitable for human habitation, and there are many relics of ancient human sites.Along with the development of tectonic movement and the change of river geomorphology, the ancient human sites have also migrated, and the tectonic movement affects the choice of the living place of the ancestors to some extent.
The study mainly studies the influence of Quaternary tectonic movements on the river landform and human activities in the middle reaches of the Yangtze River.The tectonic activities in the middle reaches of the Yangtze River during the Holocene are relatively simple, mainly due to the uplift, folds, tilting, and sinking effects. A series of tectonic movements formed the geomorphic forms of the region, mainly including plains, basins and hills. The Dongting plain and Jianghan Plain are close to the water source. The soil is fertile. The landform is more stable in the Holocene, and it is suitable for human habitation, and there are many relics of ancient human sites.Along with the development of tectonic movement and the change of river geomorphology, the ancient human sites have also migrated, and the tectonic movement affects the choice of the living place of the ancestors to some extent.
引文
[1]王岸,王国灿.构造地貌及其分析方法述评[J].地质科技情报,2005,24(4):7-13.
[2]史兴民,杜忠潮.中国构造地貌学的回顾与展望[J].西北地震学报,2006,28(6):280-284.
[3]李勇,周荣军,DENSMORE A L,等.青藏高原大陆动力学过程与地质响应[M].北京:地质出版社,2006:92-130.
[4]BURBANK D W,ANDERSON R S.Tectonic Geomorphology[M].Wiley-Blackwell Press,2012:1-17.
[5]WOBUS C,HEIMSATH A,WHIPPLE K,et al.Active outof-sequence thrust faulting in the central Nepalese Himalaya[J].Nature,2005,434(7036):1008-1011.
[6]张会平,刘少峰,孙亚平,等.基于SRTM-DEM区域地形起伏的获取及应用[J].国土资源遥感,2006(1):31-35.
[7]BRYAN K.Recent deposits of Chaco Canyon New Mexico in relation to the lives of the prehistoric peoples of Pueblo Bonito[J].Washington Academy of Science Journal,1926,16:75-76.
[8]王雯雯,王书航,姜霞,等.洞庭湖沉积物不同形态氮赋存特征及其释放风险[J].环境科学研究,2013,26(6):598-605.
[9]刘志刚,倪兆奎.鄱阳湖发展演变及江湖关系变化影响[J].环境科学学报,2015,35(5):1265-1273.
[10]李新民.长江中游地区水资源可持续利用研究[M].武汉:华中师范大学出版社,2002:1-10.
[11]BOARD M E A.Millenium Ecosystem Assessment-Ecosystems and human well-being:wetlands and water synthesis[J].Physics Teacher,2005,34(9):534-534.
[12]PARDUCC L,JORGENSEN T,TOLLEFSRUD M,et al.Glacial Survival of Boreal Trees in Northern Scandinavia[J].Science,2012,338(6108):1083-1086.
[13]BONDRE N R,KIEFER T,GUNTEN L.Paired perspectives on global change[J].Pages news,2012,20(1):1-56.
[14]MESSERLI B,MARTIN G,THOMAS H,et al.From naturedominated to human-dominated environmental changes[J].IGU Bulletin,2000,50(1):23-38.
[15]MOONEY H A,DURAIAPPAH A,LARIGAUDERI A.Evolution of natural and social science interactions in global change research programs[J].Proceedings of the National Academy of Science,2013,26(110):3665-3672.
[16]朱诚,郑朝贵,吴立,等.长江流域新石器时代以来的环境考古[M].北京:科学出版社,2015.
[17]PUMPELLY R,DAVIS W M,HUNTINGTON E.Explorations in Turkestan:with an account of the basin of eastern Persia and Sistan:expedition of 1903,under the direction of Raphael Pumpelly[M].Carnegie Institution of Washington,1905:15-26.
[18]GU Y S,WANG H L,HUANG X Y,et al.Phytolith records of the climate change since the past 15000 years in the middle reach of the Yangtze River in China[J].Frontiers of Earth Science,2012,6(1):10-17
[19]BRYAN K.Pre-Columbian agriculture in the southwest,as conditioned by periods of alleviation[J].Annals of the American Association of Geography,1941,31(4):219-242.
[20]STEARNS C E,BRYAN K.The Geology of Chaco Canyon,New Mexico,in Relation to the Life and Remains of the Prehistoric Peoples of Pueblo Bonito[J].American Antiquity,1954,21(3):324-324.
[21]HACK J T.The changing physical environment of the Hopi Indians of Arizona[J].Paper of the Peabody Museum of American Archaeology and Ethnology,1942,45(1):935-976.
[22]STEWARD J H.Theory of Culture Change:The Methodology of Multilinear Evolution[M].University of Illinois Press,1955:540-542.
[23]THORNDYCRAFT V R,Benito G,BARRIENDOS M,et al.Palaeofloods Historical Data and Climatic variability:Applications in Flood Risk Assessment[Z].Madrid:CSIC,2003.
[24]BENITO G,THORNDYCRAFT V R.Systematic Palaeoflood and Historical Data for the Improvement of Flood Risk Estimation:Methodological Guide[Z].Madrid:CSIC,2004.
[25]SMITH A M.Paleoflood hydrology of the lower Umgeni River from a reach south of the Inada Dam,Natal[J].South African Geographical Journal,1992,74(2):63-68.
[26]SMITH A M,ZAWADA P K.Palaeoflood hydrology:a tool for South Africa-an example[J].South African Journal of Geology,1994,97:21-32.
[27]ZAWADA P K.Palaeoflood hydrology:method and application in flood-prone southern Africa[J].South Africa Journal of Science,1997,93:111-132.
[28]ZAWADA P K.Palaeoflood hydrology of selected South African rivers[J].South African Geological Survey Memoir,2000,87:173-183.
[29]GREENBAUM N,ENZEL Y,SCHICK A P.Magnitude and frequency of paleofloods and historical floods in the Arava basin,NEGEV DESERT,ISRAEL[J].ISRAEL JOURNAL OF EARTH-SCIENCES,2001,50:159-186.
[30]GREENBAUM N,SCHICK A P,BAKER V R.The paleoflood record a hyperarid catchment,Nahal Zin,Negev Desert,Israel[J].Earth Surface Processes and Landforms,2015,25(9):951-971.
[31]THOMPSON R,BLOEMENDAL J,DEARING J A,et al.Environmental applications of magnetic measurements[J].Science,1980,207(4430):481-486.
[32]KOCHEL R C,BAKER V R.Paleoflood hydrology[J].Science,1982,215(4531):353-361.
[33]BAKER V R,ELY L,CONNOR J E,et al.Paleoflood hydrology and design applications[M]//SINGH V P.Regional Flood Frequency Analysis.Washington,DC:American Geophysical Union,1987:339-353.
[34]BAKER V R.Palaeoflood hydrology in a global context[J].Catena,2006,66:161-168.
[35]ZAWADA P,HATTINGH J.Studies on the palaeoflood hydrology of South African rivers[J].South African Journal of Science,1994,90:567-568.
[36]WOHL E E,GREENBAUM N,SCHICK A P,et al.Controls on bedrock channel morphology along Nahal Paran,Israel[J].Earth Surface Processes and Landforms,1994,19:1-13.
[37]LI F,ZHU C,WU L,et al.Environmental humidity changes inferred from multi-indicators in the Jianghan Plain,Central China during the last 12,700 years[J].Quaternary International,2014,349:68-78.
[38]WU L,WANG X Y,ZHOU K S,et al.Transmutation of ancient settlements and environmental changes between 6000-2000aBP in the Chaohu Lake Basin,East China[J].Journal of Geographical Sciences,2010,20(5):687-700.
[39]余文畴.长江河道演变与治理[M].北京:中国水利水电出版社,2005:10-16.
[2]史兴民,杜忠潮.中国构造地貌学的回顾与展望[J].西北地震学报,2006,28(6):280-284.
[3]李勇,周荣军,DENSMORE A L,等.青藏高原大陆动力学过程与地质响应[M].北京:地质出版社,2006:92-130.
[4]BURBANK D W,ANDERSON R S.Tectonic Geomorphology[M].Wiley-Blackwell Press,2012:1-17.
[5]WOBUS C,HEIMSATH A,WHIPPLE K,et al.Active outof-sequence thrust faulting in the central Nepalese Himalaya[J].Nature,2005,434(7036):1008-1011.
[6]张会平,刘少峰,孙亚平,等.基于SRTM-DEM区域地形起伏的获取及应用[J].国土资源遥感,2006(1):31-35.
[7]BRYAN K.Recent deposits of Chaco Canyon New Mexico in relation to the lives of the prehistoric peoples of Pueblo Bonito[J].Washington Academy of Science Journal,1926,16:75-76.
[8]王雯雯,王书航,姜霞,等.洞庭湖沉积物不同形态氮赋存特征及其释放风险[J].环境科学研究,2013,26(6):598-605.
[9]刘志刚,倪兆奎.鄱阳湖发展演变及江湖关系变化影响[J].环境科学学报,2015,35(5):1265-1273.
[10]李新民.长江中游地区水资源可持续利用研究[M].武汉:华中师范大学出版社,2002:1-10.
[11]BOARD M E A.Millenium Ecosystem Assessment-Ecosystems and human well-being:wetlands and water synthesis[J].Physics Teacher,2005,34(9):534-534.
[12]PARDUCC L,JORGENSEN T,TOLLEFSRUD M,et al.Glacial Survival of Boreal Trees in Northern Scandinavia[J].Science,2012,338(6108):1083-1086.
[13]BONDRE N R,KIEFER T,GUNTEN L.Paired perspectives on global change[J].Pages news,2012,20(1):1-56.
[14]MESSERLI B,MARTIN G,THOMAS H,et al.From naturedominated to human-dominated environmental changes[J].IGU Bulletin,2000,50(1):23-38.
[15]MOONEY H A,DURAIAPPAH A,LARIGAUDERI A.Evolution of natural and social science interactions in global change research programs[J].Proceedings of the National Academy of Science,2013,26(110):3665-3672.
[16]朱诚,郑朝贵,吴立,等.长江流域新石器时代以来的环境考古[M].北京:科学出版社,2015.
[17]PUMPELLY R,DAVIS W M,HUNTINGTON E.Explorations in Turkestan:with an account of the basin of eastern Persia and Sistan:expedition of 1903,under the direction of Raphael Pumpelly[M].Carnegie Institution of Washington,1905:15-26.
[18]GU Y S,WANG H L,HUANG X Y,et al.Phytolith records of the climate change since the past 15000 years in the middle reach of the Yangtze River in China[J].Frontiers of Earth Science,2012,6(1):10-17
[19]BRYAN K.Pre-Columbian agriculture in the southwest,as conditioned by periods of alleviation[J].Annals of the American Association of Geography,1941,31(4):219-242.
[20]STEARNS C E,BRYAN K.The Geology of Chaco Canyon,New Mexico,in Relation to the Life and Remains of the Prehistoric Peoples of Pueblo Bonito[J].American Antiquity,1954,21(3):324-324.
[21]HACK J T.The changing physical environment of the Hopi Indians of Arizona[J].Paper of the Peabody Museum of American Archaeology and Ethnology,1942,45(1):935-976.
[22]STEWARD J H.Theory of Culture Change:The Methodology of Multilinear Evolution[M].University of Illinois Press,1955:540-542.
[23]THORNDYCRAFT V R,Benito G,BARRIENDOS M,et al.Palaeofloods Historical Data and Climatic variability:Applications in Flood Risk Assessment[Z].Madrid:CSIC,2003.
[24]BENITO G,THORNDYCRAFT V R.Systematic Palaeoflood and Historical Data for the Improvement of Flood Risk Estimation:Methodological Guide[Z].Madrid:CSIC,2004.
[25]SMITH A M.Paleoflood hydrology of the lower Umgeni River from a reach south of the Inada Dam,Natal[J].South African Geographical Journal,1992,74(2):63-68.
[26]SMITH A M,ZAWADA P K.Palaeoflood hydrology:a tool for South Africa-an example[J].South African Journal of Geology,1994,97:21-32.
[27]ZAWADA P K.Palaeoflood hydrology:method and application in flood-prone southern Africa[J].South Africa Journal of Science,1997,93:111-132.
[28]ZAWADA P K.Palaeoflood hydrology of selected South African rivers[J].South African Geological Survey Memoir,2000,87:173-183.
[29]GREENBAUM N,ENZEL Y,SCHICK A P.Magnitude and frequency of paleofloods and historical floods in the Arava basin,NEGEV DESERT,ISRAEL[J].ISRAEL JOURNAL OF EARTH-SCIENCES,2001,50:159-186.
[30]GREENBAUM N,SCHICK A P,BAKER V R.The paleoflood record a hyperarid catchment,Nahal Zin,Negev Desert,Israel[J].Earth Surface Processes and Landforms,2015,25(9):951-971.
[31]THOMPSON R,BLOEMENDAL J,DEARING J A,et al.Environmental applications of magnetic measurements[J].Science,1980,207(4430):481-486.
[32]KOCHEL R C,BAKER V R.Paleoflood hydrology[J].Science,1982,215(4531):353-361.
[33]BAKER V R,ELY L,CONNOR J E,et al.Paleoflood hydrology and design applications[M]//SINGH V P.Regional Flood Frequency Analysis.Washington,DC:American Geophysical Union,1987:339-353.
[34]BAKER V R.Palaeoflood hydrology in a global context[J].Catena,2006,66:161-168.
[35]ZAWADA P,HATTINGH J.Studies on the palaeoflood hydrology of South African rivers[J].South African Journal of Science,1994,90:567-568.
[36]WOHL E E,GREENBAUM N,SCHICK A P,et al.Controls on bedrock channel morphology along Nahal Paran,Israel[J].Earth Surface Processes and Landforms,1994,19:1-13.
[37]LI F,ZHU C,WU L,et al.Environmental humidity changes inferred from multi-indicators in the Jianghan Plain,Central China during the last 12,700 years[J].Quaternary International,2014,349:68-78.
[38]WU L,WANG X Y,ZHOU K S,et al.Transmutation of ancient settlements and environmental changes between 6000-2000aBP in the Chaohu Lake Basin,East China[J].Journal of Geographical Sciences,2010,20(5):687-700.
[39]余文畴.长江河道演变与治理[M].北京:中国水利水电出版社,2005:10-16.