| 福建政和-海丰断裂带地震活动特征分析 |
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| 引用本文： | 陈秋英,陈传昌.福建政和-海丰断裂带地震活动特征分析[J].地震地磁观测与研究,2007,28(3):34-37. |
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| 作者姓名： | 陈秋英 陈传昌 |
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| 作者单位： | 中国福建,353000,南平地震台 |
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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.
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| 关 键 词： | 福建 政和-海丰断裂 地震活动 |
| 文章编号： | 1003-3246（2007）03-0034-04 |
| 收稿时间： | 2006-05-25 |
| 修稿时间： | 2006-05-25 |
Characteristics of earthquake activity of the Zhenghe-Haifeng fault zone in Fujian Province |
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| Chen Qiuying,Chen Chuanchang.Characteristics of earthquake activity of the Zhenghe-Haifeng fault zone in Fujian Province[J].Seismological and Geomagnetic Observation and Research,2007,28(3):34-37. |
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| Authors: | Chen Qiuying Chen Chuanchang |
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| Institution: | Nanping Seismic Station ,Fujian Province 353000 ,China |
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| Abstract: | 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 frequent occurrence at medium and strong level has been formed. |
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| Keywords: | Fujian Province Zhenghe-Haifeng fault zone seismic activity |
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