Response of Landform Development to the Tectonic Movement and the Climate Changes in Fenhe Drainage Basin
Received date: 2001-06-04
Revised date: 2001-09-26
Online published: 2002-05-25
Supported by
National Natural Science Foundation of China,No. 40071016
Based on analysis of the characteristics of the terraces in patterns and sediment of the Fenhe drainage basin, we find it was the three tectonic uplifts that caused the formation of three-level terraces. These uplifts took place at 0.76 MaBP, 0.55 MaBP and 0.13 MaBP respectively and resulted in the three low-level stages of the paleolake in consistent with the development of S8, S5, S1 in time. Compared with the neotectonic movements in the upper reaches of the Yellow River, the three tectonic uplifts in this region are in correspondence with them, and this may imply that the neotectonic uplifts of the Qinghai-Tibet Plateau strongly controlled the tectonic movements in the Fenhe drainage basin. According to the features of laustrine sediment deposited from the time when S5 ended its formation to the time when S1 began to develop, we also find the changes in paleoclimate from dry to wet influenced the development of the paleolakes. The lake levels rose when it was wet and dropped when it was dry, but the extent of this change of the lake levels was no more than 4.5 m, and much smaller than that caused by tectonic moveme.
HU Xiaomeng, FU Jianli, LI Youli . Response of Landform Development to the Tectonic Movement and the Climate Changes in Fenhe Drainage Basin[J]. Acta Geographica Sinica, 2002 , 57(3) : 310 -318 . DOI: 10.11821/xb200203007
[1] Yang Jingchun. The relations between the development of the paleo-rivers with neotectonic movements in Huailai Basin. Quaternary Research in China, 1965, 4(2): 93-104.
[杨景春. 怀来盆地的形成、发展及古河道演变与新构造运动的关系. 中国第四纪研究, 1965, 4(2): 93-104.]
[2] Berryman K R. Late Quaternary movement on the Wellington Fault in the Upper Hutt area, New Zealand. New Zealand Journal of Geology and Geophysics, 1990, 33: 257-270.
[3] Meyer G A, Well S G, Balling R C. Response of alluvial systems to fire and climate change in Yellowstone National Park. Nature, 1992, 357: 147-149.
[4] Nest J V et al. Postglacial response of a stream in central Iowa to changes in climate and drainage basin factors. Quaternary Research, 1990, 33: 73-85.
[5] Porter S C, An Z S, Zheng H B. Cyclic Quaternary alluviation and terracing in a non-glaciated drainage basin on the north flank of the Qingling Shan, Central China. Quaternary Research, 1992, 38: 157-169.
[6] Huang Bingwei, Zheng Du, Zhao Mingcha et al. Modern Physical Geography. Beijing: Science Press, 1999. 94-117.
[黄秉维, 郑度, 赵明茶 等. 现代自然地理. 北京: 科学出版社, 1999. 94-117.]
[7] Li Youli, Yang Jingchun. The response of the terraces in the plain of Hexi Corridor to the changes in climate during Holocene. Scientia Geographica Sinica, 1997, 17(3): 248-252.
[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.]
[8] Teihard de chardin P et al. The late Cenozoic formations of S.E. in Shanxi. Bull. Geol. Soci. China, 1933, (12).
[9] Licent E et al. The pleiocene lacustrine series in central Shanxi. Bull. Geol. Soci. China, 1935, (10).
[10] Feng Jinglan. The estimate on the ages of the stratigraphy in Shanxi Graben and central Shanxi province. Bull. Geol. Soci. China, 1933, (13).
[11] Yang Jingchun, Han Mukang, Liu Guangxun et al. The terraces and neotectonic movements in the south part of Fen River. In: The Institute of Earth Crust Stress, Chinese Seismic Bureau (ed.). The Collected Works on the Structure and Stress of Earth Crust (Vol. 1). Beijing: Seismic Press, 1987. 30-41.
[杨景春, 韩慕康, 刘光勋 等. 汾河南段河流阶地与新构造运动. 见: 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.]
[12] Pei Wenzhong, Wu Rukang, Jia Lanpo. The report on the digged paleolithes in Ding Village, Xiangfen, Shanxi. In: The second monograph from the Institute of Paleovertebrate, CAS. Beijing: Science Press, 1958. 40-45.
[裴文中, 吴汝康, 贾兰坡. 山西襄汾丁村旧石器时代遗址发掘报告. 见: 中国科学院古脊椎动物研究所甲种专刊第二号. 北京: 科学出版社, 1958. 40-45.]
[13] Wang Nailiang, Yang Jingchun, Xia Zhengkai et al. The sediment in Cenozoic and structural landform in Shanxi Graben. Beijing: Science Press, 1996. 156-200.
[王乃梁, 杨景春, 夏正锴 等. 山西地堑系新生代沉积与构造地貌. 北京: 科学出版社, 1996. 156-200.]
[14] Li Jijun, Fang Xiaomin. The research on the uplifts of Qingzang Plateau and changes in the environment. Chinese Science Bulletin, 1998, 43(5): 1569-1574.
[李吉均, 方小敏. 青藏高原隆起与环境变化研究. 科学通报, 1998, 43(5): 1569-1574.]
[15] Wu Xihao, Jiang Fuchu, Wang Sumin. The discussion on the incision of Sanmen Gorge by Yellow River. Quaternary Research, 1998, (2): 162.
[吴锡浩, 蒋复初, 王苏民. 关于黄河贯通三门峡东流入海问题. 第四纪研究, 1998, (2): 162.]
[16] Yue Leping, Xue Xiangxi. Paleomagnetism on Chinese Loess. Beijing: Geological Press, 1995. 27-70.
[岳乐平, 薛祥熙 著. 中国黄土古地磁学. 北京: 地质出版社, 1995. 27-70.]
[17] Li Youli. The study of the age of Dingcun Formation by the loess stratigraphy. Journal of Stratigraphy, 2001, 25(2): 102-106.
[李有利, 傅建利, 胡晓猛 等. 用黄土地层学方法研究丁村组的时代. 地层学杂志, 2001, 25(2): 102-106.]
[18] Dugas D D. Late Quaternary variations in the level of paleo-lake Malheur, eastern Oregon. Quaternary Research, 1998, 50: 276-282.
[19] Liu Dongsheng. Loess and Environment. Beijing: Science Press, 1985. 303-357.
[刘东生 著. 黄土与环境. 北京: 科学出版社, 1985. 303-357.]
[20] Liu Jiaqi, Cheng Tiemei, Ni Gaozhong et al. The dating of Weinan loess section and the construction of its series in time. Quaternary Research, 1994, (3): 193-200.
[刘嘉麒, 陈铁梅, 聂高众 等. 渭河黄土剖面的年龄测定及十五万年来高分辩率时间序列的建立. 第四纪研究, 1994, (3): 193-200.]
[21] Lu Houyuan, Han Jiamao, Wu Naiqin et al. The analysis on the magnetic susceptibility of modern soils in China and its paleoclimatic significance. Science in China (series B), 1994, 24(12): 1290-1297.
[吕厚远, 韩家懋, 吴乃琴 等. 中国现代土壤磁化率分析及其古气候意义. 中国科学(B辑), 1994, 24(12): 1290-1297.]
[22] Cui Zhijiu, Wu Yongqiu, Liu Gengnian et al. About "Kunlun-Huanghe Movement". Science in CHina (series D), 1998, 28(1): 53-59.
[崔之久, 伍永秋, 刘更年 等. 关于“昆仑-黄河运动”. 中国科学(D辑), 1998, 28(1): 53-59.]
/
| 〈 |
|
〉 |