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A morphometric method to determine neotectonic activity of the Weihe basin in northwestern China
Hou, JJ ; Han, MK ; Ollier, CD
刊名episodes
1997
英文摘要In order to study the Holocene activity in the down-faulted Weihe Basin, northwest China, the authors conducted a semi-quantitative morphotectonic analysis of the drainage density using topographic maps (1:50,000) and through field investigation. The results obtained have been supported by drill hole data, repeated geodetic surveying and an isopach map of Qeuaterrzaly strata. They indicate that the Holocene tectonic activity was characterized by block-faulting of the basement on different scales against a background of southward down tilting, with differential movement of small blocks. The mechanism of block movement is shear extension of the NNE-trending Fenwei Graben System under the action of right-lateral shealing. The method, if as valid as it seems in this investigation, is usefull in predicting tectonic style and geological hazard where data other than maps are lacking.; Geosciences, Multidisciplinary; SCI(E); 5; ARTICLE; 2; 95-99; 20
语种英语
内容类型期刊论文
源URL[http://ir.pku.edu.cn/handle/20.500.11897/311491]  
专题地球与空间科学学院
推荐引用方式
GB/T 7714
Hou, JJ,Han, MK,Ollier, CD. A morphometric method to determine neotectonic activity of the Weihe basin in northwestern China[J]. episodes,1997.
APA Hou, JJ,Han, MK,&Ollier, CD.(1997).A morphometric method to determine neotectonic activity of the Weihe basin in northwestern China.episodes.
MLA Hou, JJ,et al."A morphometric method to determine neotectonic activity of the Weihe basin in northwestern China".episodes (1997).
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