| 用Corioli力讨论台湾南投7．6级大震的余震强度 |
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| 引用本文： | 郭增建,吴瑾冰.用Corioli力讨论台湾南投7．6级大震的余震强度[J].灾害学,2001,16(1):35-38. |
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| 作者姓名： | 郭增建 吴瑾冰 |
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| 作者单位： | 中国地震局兰州地震研究所, |
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| 摘 要： | 台湾南投大震是震源地方一个逆掩断层错动引起的，上盘向西错动，这种断层错动的形式其Corioli力效应是使两断层盘相互挤压，因之主震发生时能量释放不彻底，余震强度较大，本文试图用Ｃorioli力效应具体讨论台湾南投大震的余震强度。
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| 关 键 词： | 南投地震 科里奥利力 地震预报 余震强度 震源机制 |
| 文章编号： | 1000-811X(2001)01-0035-04 |
Discussion on the
Aftershock Magnitude of Nantou 7.6 Earthquake in the Taiwan Island |
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| GUO Zeng-Jian,WU Jin-bing.Discussion on the
Aftershock Magnitude of Nantou 7.6 Earthquake in the Taiwan Island[J].Journal of Catastrophology,2001,16(1):35-38. |
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| Authors: | GUO Zeng-Jian WU Jin-bing |
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| Abstract: | The Natou great earthquake in the Taiwan island is caused by a dislocation of thrust in the source region with its upper wall slipping toward the west The Corioli force of this type of dislocation makes both of fault walls compress each other Therefore, the total energy does not release completely during the mainshock and the magnitudes of the aftershocks are very large An attempt to analyze the effect of Corioli force on the aftershock intentisity of the Natou great earthquake is made in this paper |
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| Keywords: | Nantou earthquake Corioli force earthquake prediction strong aftershock |
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