闽东南大陆边缘构造特征及泉州海外大震构造环境分析  

ANALYSIS ABOUT THE STRUCTURAL CHARACTERISTICS ALONG CONTINENTAL MARGIN OF SOUTHEASTERN FUJIAN AND THE STRUCTURAL SURROUNDINGS OF STRONG QUANZHOU OVERSEA EARTHQUAKE

作　　者：吕浩江[1] 雷土成[1] 陈辉琼 杨志辉[1] 

机构地区：[1]泉州基准地震台,福建省地震局地震研究所

出　　处：《西北地震学报》1995年第2期76-81,共6页Northwestern Seismological Journal

摘　　要：闽东南大陆边缘构造活动，自晚更新世以来，断裂活动以继承性差异升降作为主要特点。本文分析了１６０４年１２月２９日泉州海外８级大震与该区断裂活动的关系，并对该次大震震源断层面错动方式进行了讨论。Since late Pleistocene ,the activity of fault blocks along continental margin has beencharacterized by elevation and subsidence movements. The strong overseas earthquakeoccurring in Quanzhou on December 29,1604, related closely to fault block activity in thearea. In this paper,we analysed the relation and discussed the dislocating way of hypocentralfault surface of this strong earthquake.

关 键 词：大陆边缘 断裂构造 震源过程 地震 构造环境 

分 类 号：P315.2[天文地球—地震学]