关键词: 漳州-厦门断裂带, 活动断裂, 右行错动

Abstract: 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.

Key words: Zhangshou-Xiamen bault zone, Active fault, Dextral dislocation