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2007年3月13日福建顺昌ML4.9、ME4.7地震研究
引用本文:林松建,张颖,林琛.2007年3月13日福建顺昌ML4.9、ME4.7地震研究[J].地震地磁观测与研究,2012(3):32-36.
作者姓名:林松建  张颖  林琛
作者单位:福建省地震局地震灾害预防中心,中国福州350003
摘    要:通过对2007年3月13日福建顺昌ML4.9、4.7地震序列、震源机制解、地震烈度等震线、地震地质及发震构造、震中附近地壳P波速度结构等资料分析,结果发现:地震序列具有孤立型地震序列特征;郑坊断裂(f2)为本次地震的发震构造;北东东向的南平一宁化断裂带应作为福建省主要地震构造给予重视;顺昌一南平一带未来存在发生中强地震的可能。

关 键 词:地震序列  震源机制解  南平-宁化断裂带  发震构造  P波速度

The dissertation of Fujian Shunchang ME 4.9, 4.7 earthquakes on March 13, 2007
Lin Songjian,Zhang Ying and Lin Chen.The dissertation of Fujian Shunchang ME 4.9, 4.7 earthquakes on March 13, 2007[J].Seismological and Geomagnetic Observation and Research,2012(3):32-36.
Authors:Lin Songjian  Zhang Ying and Lin Chen
Institution:(Earthquake Administration of Fujian Province, Fuzhou 350003, China)
Abstract:Through analyzing the data of Fujian Shunchang ML 4. 9, 4. 7 earthquakes on March 13, 2007, which of seismic sequence analysis, the focal mechanism solution, isoseismal of seismic intensity, seismogeology and seismogenic structure analysis, P-wave velocity structure around the epicentre, we can generally conclude that: firstly, sequence indicates the characteristic of isolated seismic sequence. Secondly, the seismogenic structure is Zhengfang (f2) fault. Thirdly, Nanping-Ninghua fault zone should be valued as the main seismotectonics of Fujian. Finally, the moderately strong earthquake may occur in Shunchang-Nanping area in the future.
Keywords:seismic sequence  focal mechanism solution  Nanping-Ninghua fault zone  seismogenic structure  P-wave velocity
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