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[1]CI Hongjuan,YAN Dongdong,LI Youli,et al.Geomorphic Indices in the Hanyang Segment of Zhongtiaoshan Mountains, Shanxi and Its Implication for Neotectonics[J].Research of Soil and Water Conservation,2016,23(04):363-367.

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Geomorphic Indices in the Hanyang Segment of Zhongtiaoshan Mountains, Shanxi and Its Implication for Neotectonics

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 23 Number of periods: 2016 04 Page number: 363-367 Column: Public date: 2016-04-28

Title:: Geomorphic Indices in the Hanyang Segment of Zhongtiaoshan Mountains, Shanxi and Its Implication for Neotectonics

Author(s):: CI Hongjuan¹, YAN Dongdong², LI Youli¹, ZHONG Yuezhi¹, LYU Shenghua³, XIONG Jianguo¹; 1. College of Urban and Environmental Sciences, Peking University, Beijing 100871, China;
2. No.3 Geological Brigade, Hebei Provincial Geological Prospecting Bureau, Zhangjiakou, Hebei 075000, China;
3. Qingdao Institute of Marine Geology, Ministry of Land and Resources, Qingdao, Shandong 26607, China

Keywords:: geomorphic indices; Neotectonics; Zhongtiaoshan fault; river terraces

CLC:: P931

DOI:: -

Abstract:: Based on DEM data, the quantitative study on the geomorphic indices has been carried out in the Hanyang segment of Zhongtiaoshan Mountains. The indices include stream length-gradient index (SL), hack profile of river, hypsometric integral (HI), and index of drainage basin shape (BS). It is revealed that the Hanyang River Basin is in the mature phase of geomorphic evolution. Moreover, the fault activity presents a trend of increasing firstly and decreasing later from southwest to northeast. The field investigation finds that in both Pandi and Sanxin villages, the eastern terrace developed clearly while the western did not. The phenomenon indicates that the lift of eastern side of the valley is higher than the western side, which further proves the fault activity trend.

References:: [1] 王乃樑,杨景春,夏正楷,等.山西地堑系新生代沉积与构造地貌[M].北京:科学出版社,1996.
[2] 国家地震局鄂尔多斯周缘活动断裂系课题组.鄂尔多斯周边活动断裂系[M].北京:地震出版社,1988.
[3] 徐锡伟,邓起东,董瑞树,等.山西地堑系强震的活动规律和危险区段的研究[J].地震地质,1992,14(4):305-316.
[4] 苏宗正,程新原,安卫平,等.山西运城盆地的中条山断裂[M]//中国地震局地质研究所活动断裂研究(8).北京:地震出版社,2001.
[5] 程绍平,杨桂枝.山西中条山断裂带的晚第四纪分段模型[J].地震地质,2002,24(3):89-302.
[6] Li Youli,Yang Jingchun,Xia Zhengkai,et al.Tectonic geomorphology in Shanxi Graben System, Northern China[J]. Geomorphology,1998(23):77-89.
[7] 李有利,杨景春.山西运城盐湖沉积环境及其演化[J].地理研究,1994,13(1):70-75.
[8] 宋晓猛,张建云,占车生,等.基于DEM的数字流域特征提取研究进展[J].地理科学进展,2013,32(1):031-040
[9] 赵洪壮,李有利,杨景春,等.基于DEM数据的北天山地貌形态分析[J].地理科学,2009,29(3):445-449.
[10] Keller E A,Pinter N.Active Tectonics:Earthquakes,Uplift,and Landscape[M].New Jersey:Prentice Hall,2002.
[11] Hack J T.Stream-profiles analysis and stream-gradient index[J].Journal of Research of the U. S. Geological Survey,1973,1(4):421-429.
[12] Strahler A N.Hypsometric(area-altitude)analysis of erosional topography[J].Geological Society of America Bulletin,1952,63:1117-1142.
[13] Bull W B,McFadden L D.Tectonic geomorphology north and south of the Garlock fault, California[C]//Doehring D O. Geomorphology in Arid Regions.Proceedings of the Eighth Annual Geomorphology Symposium.State University of New York,Binghamton,1977.

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