Relationship between the earthquake sequences of Tangshan and Xingtai and the three dimensional velocity structure──Discussion on predicting strong earthquakes of swarm-type

被引:2
作者
梅世蓉
薛艳
尹京苑
机构
关键词
strong earthquake sequence; low-velocity anomalous body; strong swarm-type earthquake; dominant focal depth; the biggest focal depth of aftershocks;
D O I
暂无
中图分类号
P315.7 [地震观测预报];
学科分类号
070801 ;
摘要
In this paper, based on the results of tomographic image of Tangshan and Xingtai areas, the relations between thecharacteristics of the two strong earthquake sequences and their three-dimensional velocity structures are studied.The research results indicate that:① Mosaic distribution of low-velocity bodies and high-velocity bodies, especially the existence of high-velocity bodies with large size in crust are the common basis of development of thetwo earthquake sequences. ② Scale, depth, and heterogeneity of high-velocity and low-velocity bodies are theimportant factors to effect the characteristic of earthquake sequences. ③ The depth of the high-velocity body inTangshan area is less than that in Xingtai area, which is the principal reason why the dominant focal depth and thebiggest focal depth of Tangshan earthquake sequence are less than Xingtai's. ④ The depth of the high-velocitybodies in Ninghe area is more than that in Tangshan-Luanxian area, which lead to the biggest magnitude and epicentral intensity are lower. These results could be helpful for predicting the main shock of strong swarm-typeearthquakes and later strong aftershocks.
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页码:175 / 182
页数:8
相关论文
共 4 条
[2]   1966年邢台地震区地震测深资料再解释 [J].
林真明 ;
邵学钟 ;
陈学波 .
华北地震科学, 1990, (03) :55-66
[3]   1966年邢台7.2级地震的构造背景和发震构造 [J].
徐杰 ;
方仲景 ;
杨理华 .
地震地质, 1988, (04) :51-59
[4]   华北东部地区地壳结构的初步研究 [J].
孙武城 ;
李松林 ;
杨玉春 .
地震地质, 1985, (03) :1-11