| On the Occurrence Time of an Earthquake Cluster in the Shanxi Reservoir |
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| 引用本文： | Niu Anfu. On the Occurrence Time of an Earthquake Cluster in the Shanxi Reservoir[J]. 中国地震研究, 2006, 20(4): 406-411 |
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| 作者姓名： | Niu Anfu |
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| 作者单位： | Niu Anfu，Zhang Xiaodong，Zheng Dalin，Li Xiaofan and Ji PingChina Earthquake Networks Center，CEA，Beijing 100036，China |
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| 基金项目： | This research was funded by the Joint Earthquake ScienceFoundation,China (104103) |
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| 摘 要： | ![]()
INTRODUCTIONEarthquake induced byreservoir is a kind of crust motion andis an outcome of the joint functionof current crustal movement andreservoir storage .The cause of reservoir-induced earthquakesincludesthe decrease of strengthand elasticity modulus of rockonthe one hand,andthe decrease of friction offault surface because of water permeation onthe other .The more large-scale reservoirs built ,the more reservoir-induced earthquakes will happen.As iswell known,reservoir-induced earthqua…
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| 关 键 词： | 山西 水库水位 群发地震 固体潮 发生时间 |
| 收稿时间： | 2006-03-17 |
| 修稿时间： | 2006-06-02 |
On the Occurrence Time of an Earthquake Cluster in the Shanxi Reservoir |
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| Niu Anfu. On the Occurrence Time of an Earthquake Cluster in the Shanxi Reservoir[J]. Earthquake Research in China, 2006, 20(4): 406-411 |
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| Authors: | Niu Anfu |
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| Affiliation: | China Earthquake Networks Center, CEA ,Beijing 100036, China |
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| Abstract: | ![]()
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| Keywords: | Shanxi reservoir Water level Earthquake cluster Solid tide |
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