六棱山北麓中段冲沟地貌发育的定量研究及其新构造意义

doi:10.13249/j.cnki.sgs.2011.02.244

地理科学 ›› 2011, Vol. 31 ›› Issue (2): 244-250.doi: 10.13249/j.cnki.sgs.2011.02.244

六棱山北麓中段冲沟地貌发育的定量研究及其新构造意义

闫冬冬, 吕胜华, 赵洪壮, 李有利

北京大学城市与环境学院, 北京 100871

收稿日期:2010-04-19 修回日期:2010-06-07 出版日期:2011-02-20 发布日期:2011-02-20
通讯作者: 李有利,男,教授。E-mail:liyouli@pku.edu.cn E-mail:liyouli@pku.edu.cn
基金资助:
国家自然科学基金项目(40971001)、地震行业科研专项(200908001)资助。

Geomorphic Analysis and Its Implication to Neotectonics in Middle of Northern Front of Liulengshan Mountain, Northern Shanxi

YAN Dong-dong, LÜ Sheng-hua, ZHAO Hong-zhuang, LI You-li

College of Urban and Environmental Sciences, Peking University, Beijing 100871, China

Received:2010-04-19 Revised:2010-06-07 Online:2011-02-20 Published:2011-02-20

摘要/Abstract

摘要： 利用地貌形态指标对六棱山北麓断层中段的5条冲沟进行定量化研究,流域的冲沟比降指标(SL)、面积-高度积分值(HI)和流域盆地形态因子(Bs)的异常值表明5条冲沟的发育对六棱山北麓断层活动性有明显的响应,流域发育处于壮年期。秋林沟口野外实测数据验证并揭示了六棱山北麓断裂晚第四纪以来的活跃性。

Abstract: Quantitative study on the geomorphic indices has been carried out on five gullies in the middle of northern front of Liulengshan Mountain.The abnormal values of the indices, including stream length-gradient index (SL index), hypsometric integral (HI), and index of drainage basin shape (Bs), reveal that the evolution of the five gullies has obvious relationship with the neotectonic movement along the northern front of Liulengshan Mountain and the drainage basins are currently in the mature period of geomorphic evolution.The field investigation of the Qiulin gully tests demonstrates the Late Quaternary activities of the fault along the northern front of Liulengshan Mountain.

中图分类号:

P931.2

闫冬冬, 吕胜华, 赵洪壮, 李有利. 六棱山北麓中段冲沟地貌发育的定量研究及其新构造意义[J]. 地理科学, 2011, 31(2): 244-250.

YAN Dong-dong, LÜ Sheng-hua, ZHAO Hong-zhuang, LI You-li. Geomorphic Analysis and Its Implication to Neotectonics in Middle of Northern Front of Liulengshan Mountain, Northern Shanxi[J]. SCIENTIA GEOGRAPHICA SINICA, 2011, 31(2): 244-250.

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六棱山北麓中段冲沟地貌发育的定量研究及其新构造意义

Geomorphic Analysis and Its Implication to Neotectonics in Middle of Northern Front of Liulengshan Mountain, Northern Shanxi

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