摘要
依据独特的地貌景观、一系列地质体和重力场的水平错动及震源机制解等资料,论证了漳州-厦门断裂带N_2以来发生了右行错动.并进一步讨论了这种运动的性质和机制。
On the basis of data about the specific landscape,the horizontal dislocation of a series of geological bodies,and analysis of the gravitational field the facal mechanism and so on,this paper proves that dextral dislocations have occurred along Zhangzhou-Xiamen fault zone since the Tertiary.Furthermore,the nature and mechanism of this movement are also discussed.
出处
《地震地质》
EI
CSCD
北大核心
1992年第2期151-156,共6页
Seismology and Geology
关键词
漳州-厦门
断裂带
右行错动
Zhangshou-Xiamen bault zone, Active fault, Dextral dislocation
