河流阶地的形成、演变及环境效应
收稿日期: 2005-12-01
修回日期: 2006-03-01
网络出版日期: 2006-05-25
基金资助
国家重点基础研究发展计划( 973 计划) 资助( 编号: 2003CB415101) .
Formation and Evolution of River Ter r ace and Environment Responses
Received date: 2005-12-01
Revised date: 2006-03-01
Online published: 2006-05-25
魏全伟,谭利华,王随继 . 河流阶地的形成、演变及环境效应[J]. 地理科学进展, 2006 , 25(3) : 55 -61 . DOI: 10.11820/dlkxjz.2006.03.007
As one of the consequences of historical fluvial evolution, river terrace has recorded some information about environmental changes during river processes. It is the significant geomorphologic complex for analyzing river' s historical evolution. This work gives a review on the origin, geomorphologic characteristics, causes of formation, environment responses and the datemeasure technology of river terraces as well as its significance in reconstruction of environment during terrace formation. It shows that river terraces are the integrative consequence of the river system and related environment influences. Researchers should consider the entire river system and its environment syntheses to study river terraces. The geological tectonic and climate characteristics and ancient river dynamics may be revealed according to research of river terraces. River terraces are the crucial geomorphologic elements used to reveal the environmental information in study areas. With the development of the meterage instruments, the date - measure technology will be more accurate and sensitive. The dynamic simulation and the quantitative analysis for the formation and evolution of river terraces need more exploration.
[1] Bull W B. Thresh shold of critical power in streams, Geological Society of America Bulletin, 1979, 90(5): 453~464.
[2] Brakenridge G R. Late Quaternary Floodplain Sedimentation along the Pommede Terre River, Southern Missouri, Quaternary Research, 1981, 15(1): 62~76.
[3] 沈玉昌, 龚国元. 河流地貌学概论, 北京·科学出版社, 1986: 56~71, 85~153.
[4] Fuller I C, etc. River Response to High Frequency Climate Oscillations in Southern Europe Over the Past 2000K.y, Geology, 1998, 26(3): 275~278.
[5] 杨景春, 李有利. 地貌学原理. 北京:北京大学出版社, 2001: 1~230.
[6] Chatters J C, Hoober K A. Response of the Columbia River Fluvial System to Holocene Climate change, Quaternary Research, 1992, 37:42~59.
[7] 郑文涛, 杨景春, 段锋军. 威武盆地晚更新世河流阶地变形与新构造运动. 地质地震, 2000, 22(3): 318~328.
[8] 史兴民, 杨景春. 河流地貌对构造运动的响应. 水土保持研究, 2003, 10(3): 48~51.
[9] 胡小猛, 傅建利, 李有利. 汾河流域地貌发育对构造运动和气候变化的响应. 地理学报, 2002, 57(3): 317~324.
[10] 李有利, 谭利华, 段烽军, 杨景春. 甘肃酒泉盆地河流地貌与新构造运动. 干旱区地理, 2000, 23(4): 304~309.
[11] 陆中臣, 贾绍凤, 黄克新, 元宝印. 流域地貌系统. 大连:大连出版社, 1991, 77~107, 166~272, 313~336, 351~356.
[12] 冯起, 李振山, 陈广庭. 国外干旱区河流地貌研究综述. 地理研究, 1997, 16(2): 89~95.
[13] Chappell J. A revised sea level record for the last 300 000 years from Papua Guinea, Search, 1983, 14(3~4): 99~101.
[14] Brakenridge G R. Wide Spread Episodes of Stream Erosion during the Holocene and their Climatic Cause, Nature, 1980,(283): 655~656.
[15] 周厚云, 高全洲, 朱照宇, 郭国章. 气候环境变化的河流响应. 中山大学学报( 自然科学版) , 2001, 40(6): 81~85.
[16] 刘小凤, 刘百篪. 应用“构造- 气候旋回”年代方法确定河流阶地形成年代的初步研究. 西北地震学报, 2003, 23(4): 395~403.
[17] 王永, 王军, 迟振卿, 肖序常, 张招崇. 克里雅河阶地的形成与西昆仑山隆升. 宁夏工程技术, 2004, 3(3): 207~209.
[18] Burnett A W, Schumm S A. Alluvial- river Response to Neotectonic Deformation in Louisiana and Mississippi, Science, 1983, (222): 49~50.
[19] Hsieh, Meng- long, Knuepfer, P L K. Middle- late Holocene River in the Erhjen River Basin, Southwestern Taiwan- Implications of River to Climate Change and Active Tectonic Uplift, Geomorphology, 2001, 38(3~4): 337~372.
[20] Antoine, P. Lautridou, J. P. Laurent, M. Long- term Fluvial Archives in NW France: Response of Seine and Somme River to Tectonic Movements, Climatic Variation and Sea- level Changes, Geomorphology, 2000, 33(3~4): 183~207.
[21] Maddy, D. Bridgland, D. R. Green, C. P. Crustal Uplift in Southern England: Evidence from the River Terrace Records, Geomorphology, 2000, 33(3~4): 167~181.
[22] 李吉均, 方小敏, 马海洲, 朱俊杰, 潘保田, 陈怀录. 晚新生代黄河上游地貌演化与青藏高原隆起. 中国科学(D 辑) , 1996, 26(4): 316~322.
[23] 杨达源, 吴胜光, 王云飞. 黄河上游的阶地与水系变迁. 地理科学, 1996, 16(2): 137~143.
[24] 王岸, 王国灿, 向树元. 东昆仑山东段北坡河流阶地发育及其与构造隆升的关系. 地球科学- 中国地质大学学报, 2003, 28(6): 675~679.
[25] 史兴民, 杨景春, 李有利, 南峰. 天山北麓玛纳斯河河流阶地变形与新构造运动. 北京大学学报( 自然科学版) , 2004, 40(6): 971~978.
[26] 陈杰, 卢演俦, 丁国瑜. 祁连山西段酒西盆地区阶地构造变形的研究. 西北地震学报, 1998, 20(1): 28~36.
[27] Youli Li, Jingchun Yang, Zhengkai Xia etal. Tectonic geomorphology in the Shanxi Graben System, Northern China, Geomorphology, 1998, 23: 77~89.
[28] 杨景春, 谭利华, 李有利, 段烽军. 祁连山北麓河流阶地和新构造演化. 第四纪地质, 1998, (3): 229~237.
[29] 李长安, 殷鸿福, 于庆文, 黄长生. 昆仑山东段的构造隆升. 水系响应与环境变化, 地球科学- 中国地质大学学报, 1998, 23(5): 456~460.
[30] 曾永年, 马海洲, 李珍, 李玲琴. 西宁地区湟水阶地的形成与发育研究. 地理科学, 1995, 15(3): 253~258.
[31] 杨景春, 韩慕康, 刘光勋. 汾河南段河流阶地与新构造运动, 国家地震局地壳应力研究所编, 地壳构造与地壳应力文 集( 一) . 北京·地震出版社, 1987, 30~41.
[32] 袁庆东, 郭召杰, 张志诚, 吴朝东, 张锐, 方世虎, 王美娜. 天山北麓塔西河河流阶地的变形特征及成因探讨. 新疆地 质, 2004, 22(1): 13~16.
[33] 李有利, 杨景春. 河西走廊平原区全新世河流阶地对气候变化的响应. 地理科学, 1997, 17(3): 248~252.
[34] 郑本兴, 马秋华. 贡嘎山地区全新世的冰川变化, 气候变化与河谷阶地发育. 地理学报, 1994, 49(6): 500~508.
[35] 尹国康. 河流地貌系统的信息反馈. 南京大学学报, 1994, 30(2): 344~352.
[36] 陈铁梅. 第四纪测年的进展与问题. 第四纪研究, 1995, (2): 182~191.
[37] 孙红艳, 李志祥, 田明中. 第四纪测年研究新进展. 地质力学学报, 2003, 9(4): 371~378.
[38] Aitken, M. J. Optical Dating, Quaternary Science Review, 1992, (11): 127~131.
[39] Huntrley, D. J. Godfrey- Smith, D. I. Thewalt, M. L. W. Optical Dating of Sediments, Nature, 1985, (313): 105~107.
[40] Zimmerman, D. W. Thermoluminescence from fine grains from ancient, Archaeometry, 1967,10: 26~28.
[41] 李保俊, 杨景春, 李有利. 根据砾石风化圈厚度估算地貌年龄. 地理研究, 1996, 15(1): 11~21.
[42] 彭子成. 第四纪测年的新技术———热电离质谱铀系法的发展近况. 第四纪研究, 1997, (3): 258~264.
[43] 邵雪梅. 树轮年代学的若干进展. 第四纪研究, 1997, (3): 265~271.
/
| 〈 |
|
〉 |