The deformation types of active faults in unconsolidated sediments and   their implication for recognizing rupture events

CORC > 北京大学 > 地球与空间科学学院

	The deformation types of active faults in unconsolidated sediments and their implication for recognizing rupture events
	Hou, JJ ; Bai, TX ; Liang, HH ; Liu, XD
刊名	zeitschrift fur geomorphologie
	1999
英文摘要	Seismic rupture produced by active faulting made ground surface fracturing and buildings seriously destroying. However, the fracturing traces are usually indistinct or invisible because of complicated deformations in Quaternary unconsolidated materials. This paper approaches the deformation types of active faults in different unconsolidated sediments by the investigation in the Weihe basin and Datong Basin, two major basins of the Feiwei graben system, China.; Geography, Physical; Geosciences, Multidisciplinary; SCI(E); 0; ARTICLE; 3; 383-391; 43
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/311471]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	Hou, JJ,Bai, TX,Liang, HH,et al. The deformation types of active faults in unconsolidated sediments and their implication for recognizing rupture events[J]. zeitschrift fur geomorphologie,1999.
APA	Hou, JJ,Bai, TX,Liang, HH,&Liu, XD.(1999).The deformation types of active faults in unconsolidated sediments and their implication for recognizing rupture events.zeitschrift fur geomorphologie.
MLA	Hou, JJ,et al."The deformation types of active faults in unconsolidated sediments and their implication for recognizing rupture events".zeitschrift fur geomorphologie (1999).