| 1918年南澳地震的破坏强度及震中位置 |
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| 引用本文： | 潘建雄,黄日恒.1918年南澳地震的破坏强度及震中位置[J].华南地震,1994,14(2):17-23. |
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| 作者姓名： | 潘建雄 黄日恒 |
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| 作者单位： | 广东省地震局 |
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| 摘 要： | 对１９１８年南澳地震的记录史料及有关文章进行了比较研究，并根据现场地震地质考察中发现的山体滑塌和地表破坏现象及其它宏观资料，重新圈定了这次地震的Ｘ度极震区，其形状为一北西向的长椭圆形，其内的北西向断裂带，应是该次地震的发震断裂。
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| 关 键 词： | 地震烈度 发震构造 震中位置 地震 |
TO DISCUSS THE DAMAGE INTENSITY AND THE EPICENTRAL LOCATION OF NANAO EARTHQUAKE IN 1918 |
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| Pan Jianxiong,Huang Riheng.TO DISCUSS THE DAMAGE INTENSITY AND THE EPICENTRAL LOCATION OF NANAO EARTHQUAKE IN 1918[J].South China Journal of Seismology,1994,14(2):17-23. |
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| Authors: | Pan Jianxiong Huang Riheng |
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| Abstract: | In this paper,the historical records and documents of Nanao Large Earthquake in 1918 have been compared,and the meizoseismal region of intensity X of this earthquake has been delineated again based on the hill-creep,the failure of ground surface and the other macrodata that had been found during seismic-geologic investigating in the field,the figure deliniated is a prolate ellipsoid in NW direction,and the NW fault zone inside the ellipsoid should be the statutory of this large earthquake. |
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| Keywords: | Nanao earthquake Damage intensity seismic intensity statutory Epicentral location |
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