Longling-Lancang fault zone in southwest Yunnan, China - A newly-generated rupture zone in continental crust

被引:13
作者
Guo, SM [1 ]
Xiang, HF
Zhou, RQ
Xu, XW
Dong, XQ
Zhang, WX
机构
[1] China Seismol Bur, Inst Geol, Beijing 100029, Peoples R China
[2] Seismol Bur Yunnan Prov, Kunming 650041, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2000年 / 45卷 / 04期
关键词
southwest Yunnan; fault zone; newly-generated rupture zone;
D O I
10.1007/BF02909774
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 [理学]; 0710 [生物学]; 09 [农学];
摘要
The Longling-Lancang fault zone, consisting of sets of en echelon or clustered faults, is a newly-generated rupture zone. It is characterized by the distribution of active faults, earthquake faults and earthquakes in zones. Formed in the Early-Middle Pleistocene, still active in the late, it moves dextrally and extensionally. It tends to cut off the locked segments and discontinuous segments at first, then pervades totally along the zone, accompanied by strong earthquakes.
引用
收藏
页码:376 / 379
页数:4
相关论文
共 6 条
[1]
CHENG L, 1979, 1976 LONGLING EARTHQ
[2]
GUO SM, 1995, RES ACTIVE FAULT, V4, P28
[3]
JIANG K, 1993, 1988 LANCANG GENGMA, P299
[4]
Yu W.-X., 1991, SEISMOLOGY GEOLOGY, V13, P343
[5]
Zhou R Q, 1998, SEISMOLOGY GEOLOGY, V20, P261
[6]
Zhou R.-Q., 1990, SEISMOLOGY GEOLOGY, V12, P291