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| 浑江断裂带现今地震活动特征分析 | |
| 引用本文： | 姜齐武,张凤楼,焦伟,程庆本,盘晓东.浑江断裂带现今地震活动特征分析[J].东北地震研究,2001,17(4):17-20. |
| 作者姓名： | 姜齐武 张凤楼 焦伟 程庆本 盘晓东 |
| 作者单位： | 1. 吉林省通化市地震局,吉林,通化,134001 2. 吉林省通化地震台,吉林,通化,134000 3. 吉林省地震局,吉林,长春,130022 |
| 摘 要： | 系统分析1977年以来浑江断裂带的地震活动资料表明，该断裂带上地震活动表现为空间上两端集中分布与震中的跳跃式迁移，发震时间分布上有明显的分段差异性及震源浅、震害大等特征。 |
| 关 键 词： | 浑江断裂带 地震活动 震中 |
| 文章编号： | 1004-2865(2001)04-0017-04 |
| 修稿时间： | 2001年4月1日 |
PERSENT SEISMIC ACTIVITY CHARACTERISTICS OF THE HUNJIANG FAULT ZONE |
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| JIANG Qi-wu,ZHANG Feng-lou,JIAO Wei,CHENG Qing-ben,Pan Xiao-dong.PERSENT SEISMIC ACTIVITY CHARACTERISTICS OF THE HUNJIANG FAULT ZONE[J].Seismological Research of Northeast China,2001,17(4):17-20. | |
| Authors: | JIANG Qi-wu ZHANG Feng-lou JIAO Wei CHENG Qing-ben Pan Xiao-dong |
| Institution: | JIANG Qi-wu 1),ZHANG Feng-lou 2),JIAO Wei 2),CHENG Qing-ben 1),Pan Xiao-dong 3 |
| Abstract: | The systematical analyzation of seismic activities along the Hunjiang fault zone since 1977 shows that the earthquakes often occur at the two ends of the fault,and the epicetres often skip from one to another,the origin times have a feature of obvious sectional differences,in addition,the earthquake sources are shallow,and the seismic hazard is very big in general. |
| Keywords: | The HunJiang fault zone Seismic activity Epicentre |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |