| 1614年平遥6?级地震参数探讨研究 |
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| 引用本文： | 马秀芳,安卫平,王跃杰.1614年平遥6?级地震参数探讨研究[J].震灾防御技术,2015,10(4):953-960. |
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| 作者姓名： | 马秀芳 安卫平 王跃杰 |
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| 作者单位： | 山西省地震局,太原 030002 ; 太原大陆裂谷动力学国家野外科学观测研究站,太原 030025;山西省地震局,太原 030002 ; 太原大陆裂谷动力学国家野外科学观测研究站,太原 030025;山西省地震局,太原 030002 ; 太原大陆裂谷动力学国家野外科学观测研究站,太原 030025 |
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| 基金项目： | 地震行业科研专项项目“历史地震资料补遗、可靠性及工程应用研究”（200708048） |
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| 摘 要： | 本文收集了1614年平遥6?级地震的各版本地震目录的参数、记录此次地震的历史史料、关于该地震的研究文献,对比了山西断陷盆地的12次5.2级至6?级历史地震和现代地震的破坏情况及有感范围,得出了此次地震的震级偏大,定为5?级更为合适的结论。同时,在前人对该地震震中参数研究的基础上,运用地震参数校订的新方法,重点定量分析了平遥一带仪器记录的小震空间分布、震群分布和地震密集值分布特征,并结合平遥一带断裂分布特征,综合分析讨论了平遥地震的震中参数。
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| 关 键 词： | 参数 历史地震 平遥 |
| 收稿时间： | 2015/2/26 0:00:00 |
Discussion about the Parameters of Pingyao Earthquake in 1614 |
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| Ma Xiufang,An Weiping and Wang Yuejie.Discussion about the Parameters of Pingyao Earthquake in 1614[J].Technology for Earthquake Disaster Prevention,2015,10(4):953-960. |
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| Authors: | Ma Xiufang An Weiping and Wang Yuejie |
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| Institution: | Earthquake Administration of Shanxi Province, Taiyuan 030002, China ; National Scientific Field Observatory of Continental Rift Dynamics in Taiyuan, Taiyuan 030002, China;Earthquake Administration of Shanxi Province, Taiyuan 030002, China ; National Scientific Field Observatory of Continental Rift Dynamics in Taiyuan, Taiyuan 030002, China;Earthquake Administration of Shanxi Province, Taiyuan 030002, China ; National Scientific Field Observatory of Continental Rift Dynamics in Taiyuan, Taiyuan 030002, China |
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| Abstract: | In this paper, we reviewed the parameters from various versions of the earthquake catalog, and the historical materials of the Pingyao earthquake in 1614.Through comparing the destructions caused by other historical or modern earthquakes with magnitude from 5.2 to 6.5 in the Shanxi basin we believed that it is more reasonable to define the magnitude of this earthquake as 5?. On the basis of previous research on this earthquake, we applied a new method of seismic parameters revision, focusing on quantitative analysis of spatial distribution of small to moderate instrumental record earthquakes, earthquake swarm features, earthquake densely value distribution. Combined with fracture distribution in the Pingyao area, we discussed the epicenter parameters of the Pingyao earthquake comprehensively. |
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| Keywords: | Parameters Historical earthquake Pingyao |
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