台湾地区强震成丛性活动初探
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摘要
文中探讨了我国台湾地区(北纬21.5°~25.5°,东经119.5°~123.0°)自1900年以来5次明显的强震成丛性活动现象,每次成丛性强震活动高潮期的能量释放持续时间由几个月至4年多不等,丛与丛间的间隔时间也各不相同,两者之间似存在着互补的关系。研究认为,这种强震成丛性活动不仅与该区所处的特殊地理环境与构造条件密切相关,还可能与大陆及周沿地区8级以上的巨大地震有关。
In this paper, the author discusses 5 times of strong earthquake activity in cluster way obviously from 1900 to nowadays in Taiwan area (21.5°~25.5°N, 119.5°~123.0°E), the duration of the climax of these strong earthquake activity was different from several months to almost 4 years, the interval of clusters was different too, and there was a complementary relation between duration and interval. These phenomena are related not only to the special geographical environment and tectonics condition, but also to the great earthquake with M8 around the area.
引文
[1] 国家地震局震害防御司.中国历史强震目录[M].北京:地震出版社,1995.中国地震局震害防御司.中国近代地震目录[M].北京:中国科学技术出版社,1999.
    [2] 李善邦.中国地震[M].北京:地震出版社,1981.
    [3] 李志雄,高旭,李宝生.中国大陆6级地震丛式活动特性分析[J].地震,1991,11(4):9 19.
    [4] 张国民,刘蒲雄,陈修启.高潮期中成串强震间的相互关系及其机理探讨[J].地震,1991,11(3):1 11.
    [5] 高旭,刘滨兴.全球地震活动与宇宙环境的关系[J].地震,1981,1(3):2 4.

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