| 地核反射之剪力波触发余震:以四川地震为例(英文) |
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| 引用本文： | 林正洪,Wen-Yen Chang. 地核反射之剪力波触发余震:以四川地震为例(英文)[J]. 国际地震动态, 2010, 0(6): 30-30. DOI: 10.3969/j.issn.0235-4975.2010.06.029 |
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| 作者姓名： | 林正洪 Wen-Yen Chang |
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| 作者单位： | 林正洪,Cheng-Horng Lin(Institute of Earth Sciences, Academia Sinica, Taipei 115);Wen-Yen Chang,Wen-Yen Chang(Science Council, Taipei 106) |
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| 摘 要： | Since the Earth outer core is liquid, the shear waves that are generated by a large earthquake and traveling to the core (ScS) will totally reflect with strong seismic energy.
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| 关 键 词： | 地核 剪力波 余震 四川 地震 |
A large aftershock of the 2008 Sichuan earthquake (MW=7.9) triggered by shear waves reflected from the earth core |
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| Cheng-Horng Lin,Wen-Yen Chang. A large aftershock of the 2008 Sichuan earthquake (MW=7.9) triggered by shear waves reflected from the earth core[J]. Recent Developments in World Seismology, 2010, 0(6): 30-30. DOI: 10.3969/j.issn.0235-4975.2010.06.029 |
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| Authors: | Cheng-Horng Lin Wen-Yen Chang |
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| Affiliation: | 1. Institute of Earth Sciences, Academia Sinica, Taipei 115
2. Science Council, Taipei 106 |
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| Abstract: | Since the Earth outer core is liquid, the shear waves that are generated by a large earthquake and traveling to the core (ScS) will totally reflect with strong seismic energy. |
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