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首页> 外文期刊>Doklady Earth Sciences >Seismicity of the Central Kuril Islands before and after the catastrophic M=8.3 (November 15, 2006) and M=8.1 (January 13, 2007) earthquakes
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Seismicity of the Central Kuril Islands before and after the catastrophic M=8.3 (November 15, 2006) and M=8.1 (January 13, 2007) earthquakes

机译:M = 8.3(2006年11月15日)和M = 8.1(2007年1月13日)大地震前后的千岛群岛中部地震

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摘要

The data on foreshocks and aftershocks of the strongest earthquakes occurred in the area of Kuril island arc on November 15, 2006 (M (w) = 8.3) and January 13, 2007 (M (w) = 8.1) are compared. In 2006, two months before the catastrophic earthquake in November, the detailed seismological investigations were carried out with the use of bottom stations in the area of seismic gap in the Central Kuril arc. The maps of epicenters and vertical cross sections for the equal time intervals are compared. The clear difference between distributions of hypocenters in the periods of foreshocks and aftershocks is revealed. Earthquakes were not distributed within the limits of the seismoactive block in the Kuril arc during the foreshocks period; instead, boundaries of seismoactive zone abruptly narrowed and hypocenters concentrated largely within the Benioff zone.
机译:比较了2006年11月15日(M(w)= 8.3)和2007年1月13日(M(w)= 8.1)在千岛群岛弧地区发生的最强烈地震的前震和余震数据。 2006年,也就是11月灾难性地震发生的前两个月,在千岛中央弧段的地震缝隙区域利用底部测站进行了详细的地震学调查。比较了相等时间间隔的震中和垂直横截面图。揭示了前震和余震期间震源分布的明显差异。在前震时期,地震没有在千岛弧的地震活动块的范围内分布。相反,地震活动带的边界突然变窄,震源主要集中在贝尼奥夫带内。

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  • 来源
    《Doklady Earth Sciences》 |2015年第2期|1101-1105|共5页
  • 作者单位

    Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia;

    Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia;

    Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia;

    Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia;

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