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Dynamics of the seismicity of the Kuril arc based on multivariate statistical analysis

机译:基于多元统计分析的千岛弧地震活动性

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The spatial-temporal distributions of earthquakes in the Kuril-Okhotsk region were analyzed. The events with Ms ≥ 4 from 1980 until 2009 and Ms ≥ 7 from 1910 until 2009 (20576 and 76 earthquakes, respectively) were studied. The specially developed program complex allowed us to obtain the 4-D distribution of the seismic events (along the sections, depths, temporal intervals, and energetic levels). It was shown that the seismic events obviously tend to cluster both along the surface and depth directions. The spatial-temporal analysis of the events (with Ms ≥ 4) in six five-year intervals from 1980 until 2009 has revealed a cyclic increase and decrease in the seismic activity in different time intervals and its cyclic migration from the South through the Central to the North Kuriles and back. The analysis of the strong events with Ms ≥ 7 in twenty 5-year intervals during 1910-2009 has shown that their amount significantly decreased for the last 30 years and the location of the hypocenter depths also changed (only shallow-focus earthquakes have been observed since 1975). The peaks of the seismic activity (1915-1919, 1955-1969, and 2005-2009) are separated by 35-year periods of its decrease.
机译:分析了千岛—鄂霍次克地区地震的时空分布。研究了1980年至2009年Ms≥4和1910年至2009年Ms≥7的事件(分别为20576和76次地震)。专门开发的程序集使我们能够获得地震事件的4维分布(沿剖面,深度,时间间隔和高能级)。结果表明,地震事件显然倾向于沿地表和深度方向聚集。从1980年到2009年的六个五年间隔内事件(Ms≥4)的时空分析表明,地震活动在不同时间间隔内呈周期性增加和减少,并且从南部到中部再到中部,呈周期性迁移。北千岛群岛,然后返回。对1910-2009年间每隔5年间隔Ms≥7的强地震的分析表明,在过去30年中,它们的数量显着减少,震源深度的位置也发生了变化(仅观测到浅震)自1975年以来)。地震活动的高峰(1915-1919、1955-1969和2005-2009)之间相隔35年。

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