福建政和-海丰断裂带地震活动特征分析
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摘要
通过对1971年以来福建政和-海丰断裂地震活动特征分析,认为政和-海丰断裂的地震活动是:在主体北东向政和-海丰断裂带和次级北西向永安-晋江断裂带相互交汇的构造格局下,形成了4~5级中强地震反复发生的潜在震源区。
Through the characteristics analysis on the earthquake activity of Zhenghe-Haifeng fault zone,it is found that under the interacting structure between the primary cracking section of Zhenghe-Haifeng fault,which is in northeast orientation,and secondary cracking section of Yongan-Jinjiang,which is towards the northwest,the potential earthquake source of fre- quent occurrence at medium and strong level has been formed.
引文
林思诚,彭美凤,张仰中等.1997.水口水库诱发地震的发展趋势及防震减灾对策研究[R].福建省地震局,15
    黄向荣,刘玉森,龙清风等.2000.福建省地震现场调查报告汇编[J].福建地震,12,1~78
    魏柏林,冯绚敏,陈定国等.2001.东南沿海地震活动特征[M].北京;地震出版社,302~352

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