| 走滑断裂的枢纽运动是形成特征地震的一种机制 |
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| 引用本文： | 王华林 耿杰. 走滑断裂的枢纽运动是形成特征地震的一种机制[J]. 地震地质, 1990, 12(1): 57-62 |
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| 作者姓名： | 王华林 耿杰 |
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| 作者单位： | 山东省地震局(王华林)，山东省地震局(耿杰) |
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| 摘 要： | 本文通过特征地震特点与枢纽运动特征的对比分析,得出走滑断裂的枢纽运动是形成特征地震的一种机制,断裂的枢纽轴部是特征地震发生的位置。研究结果表明,富蕴、海原、炉霍和郯城地震断裂皆属特征地震断裂
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| 关 键 词： | 走滑断裂 枢纽运动 枢纽轴 特征地震 |
A MECHANISM OF THE FORMATION OF CHARACTERISTIC EARTHQUAKE CAUSED BY THE PIVOTAL MOVEMENT OF STRIKE-SLIP FAULT |
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| Wang Hua-lin and Geng Jie. A MECHANISM OF THE FORMATION OF CHARACTERISTIC EARTHQUAKE CAUSED BY THE PIVOTAL MOVEMENT OF STRIKE-SLIP FAULT[J]. Seismology and Geology, 1990, 12(1): 57-62 |
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| Authors: | Wang Hua-lin and Geng Jie |
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| Affiliation: | Seismological Bureau of Shangdong Province |
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| Abstract: | Based on the analysis and comparison of the features of characteristic earthquake and pivotal movement, it is concluded that the pivotal movement of strike-slip fault leads to the occurence of characteristic earthquake, and that the pivotal axis of the fault is the site of earthquake occurence.The result also shows that the Fuyun, Luhuo, Haiyuan and Tancheng faults are the seismogenic faults of characterstic earthquake. |
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| Keywords: | Strike-slip fault Pivotal movement Pivotal axis Characteristic earthquake |
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