[1]常直杨,王建,白世彪,等.白龙江流域河流纵剖面与基岩侵蚀模型特征[J].山地学报,2015,(02):183.
 CHANG Zhiyang,WANG Jian,et al.Morphotectonic Analysis of the Bailongjiang Drainage Basin[J].Mountain Research,2015,(02):183.
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白龙江流域河流纵剖面与基岩侵蚀模型特征()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年02期
页码:
183
栏目:
山地研究
出版日期:
2015-04-01

文章信息/Info

Title:
Morphotectonic Analysis of the Bailongjiang Drainage Basin
作者:
常直杨;王建;白世彪;张志刚;
南京师范大学地理科学学院;南京旅游职业学院;南京师范大学虚拟地理环境教育部重点实验室;
Author(s):
CHANG ZhiyangWANG Jian BAI ShibiaoLIANG Zhong
1.School of Geography Science, Nanjing Normal University, Nanjing, Jiangsu 210046,China; 2. Key Laboratory of Virtual Geographical Environment(Ministry of Education), Nanjing Normal University,China; 3. Nanjing Institvte of Tourism & Hospitalvty,Nanjing 211100,China
关键词:
白龙江构造运动河流纵剖面基岩侵蚀模型陡峭指数凹曲度
Keywords:
Bailongjiang tectonic activity longitudinal profile streampower incision model concavity index steepness indices
分类号:
P931.2,P542
文献标志码:
A
摘要:
构造地形指标的发展对于构造运动的量化研究具有重要意义。白龙江流域位于青藏高原与西秦岭造山带之间的过渡地带,对该流域地貌是否处于构造隆升与河流侵蚀的均衡状态,以及内部构造活动性的差异如何等问题尚缺乏细致研究。基于Arcgis9.3与ASTERGDEM数据,提取了白龙江流域32条支流的纵剖面,拟合其最佳函数形态,并利用基岩侵蚀模型提取了各个支流的标准化陡峭指数、凹曲度及拟合系数值,来揭示白龙江流域河流对构造运动的响应特征。结果表明:白龙江流域河流拟合函数以指数函数为主,河流大多发育处于侵蚀作用强烈阶段;中上游地区标准化河流陡峭指数值较下游地区偏大,凹曲度值和拟合系数中上游较下游值偏小,反映了白龙江...
Abstract:
Geomorphic indices have been widely used for studying relative active tectonics. The research about tectonic activity can be quantified with the development of mathematical models for river and streampower incision model. Bailongjiang drainage system is located in the transition area between Tibetan Plateau and West Qinling Mountain.There is little research about this drainage basin on that whether it is in a steadystate or what is the difference about the activity. We carry out a study on the longitudinal profile of the 32 rivers, by fitting the characteristics of the river longitudinal profile using four function patterns, and analyzing the evolution process of the 32 river’s longitudinal profile based on the streampower incision model.We can concluded that tectonic activity play an important role in this region’s geomorphic indices and the upwardconvex features of the profiles, the evolution phase of the river topographic form have not got to the steady state.

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备注/Memo

备注/Memo:
收稿日期(Received date):2013-09-01;修回日期(Accepted):2013-12-11。
基金项目(Foundation item):国家自然科学基金资助项目(40871010)。[Supported by National Nature Science Foundation of China (40830742).]
作者简介(Biography):常直杨(1987-),男,河南济源人,博士研究生,从事GIS在地貌研究中的应用研究。[Chang Zhiyang(1987-),male,was born in Jiyuan,Henan Province,Ph D student,major in the study of geomorphology with GIS.] E-mail:changzhiyang1@126.com *
通信作者(Corresponding author): 王建(1962-),男,博士,教授,主要从事地貌演化发展研究。[Wangjian (1962- ),male,Dr,& professor,mainly engaged in the study of evolution of geomorphology.] E-mail: jwang169@vip.sina.com
更新日期/Last Update: 1900-01-01