| 张北6.2级地震序列特征 |
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| 引用本文： | 李淑莲,戴英华.张北6.2级地震序列特征[J].华北地震科学,1998,16(3):28-33. |
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| 作者姓名： | 李淑莲 戴英华 |
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| 作者单位： | 河北省地震局!石家庄，050021 |
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| 摘 要： | １９９８年１月１０日张北６．２级地震后，我们根据《地震现场工作大纲和震情分析指南》用ｂ值ｈ值、ｕ值，ｋ值对该次地震序列进行了综合判定。结果认为此次地震为主震余震型。张北地震序列在衰减过程中出现以４级地震为峰值有节律的起伏，在时间上有较规则的准周期，且每一组起伏前密集－平静规律十分明显。
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| 关 键 词： | 张北地震 地震序列 余震型序列 h值 ui指数 |
CHARACTERISTICS OF ZHANGBEI M6. 2 EARTHQUAKE SEQUENCE |
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| Li Shulian,Dai Yinghua,Liu Zhihui.CHARACTERISTICS OF ZHANGBEI M6. 2 EARTHQUAKE SEQUENCE[J].North China Earthquake Sciences,1998,16(3):28-33. |
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| Authors: | Li Shulian Dai Yinghua Liu Zhihui |
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| Abstract: | After the Zhangbei M6. 2 earthquake on January 10, 1998,comprehensive judgement was made for the earthquake sequence by b value,h value,u value and k value. The result considered that the earthquake belongs to main shock aftershock type. The Zhangbei earthquake sequence showed regular fluctuations with earthquake of magnitude 4 as peak value in attenuation process,showed relateively regular quasi-period in time and the concentration-quiet law is quite obvious before each group fluctuation. |
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| Keywords: | earthquake sequence main shock after shock type sequence h value u index |
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