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首页> 外文期刊>Earthquake Research in China >The Characteristics of Seismic Activity Before the Devastating Earthquake with M_W9.0 Off the West Coast of Northern Sumatra
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The Characteristics of Seismic Activity Before the Devastating Earthquake with M_W9.0 Off the West Coast of Northern Sumatra

机译:苏门答腊岛北部西海岸M_W9.0级特大地震前的地震活动特征

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The characteristics of seismic activity in different time-spatial domain before the M_W9.0 earthquake were studied. The results are as follows:①The activity of the deep earthquakes in the north boundary zone of the Australian plate had been evidently strengthened since 1994, showing an increased frequency, magnitude and depth, especially in regards to the heterogeneous distribution of the earthquake depth (namely between 500km and 689km). Meanwhile the shallow earthquakes of M ≥ 7.0 in the Sumatra island and its vicinity had been obviously strengthened too, and formed a strengthening area with a length of about 1000 km and width 300 km. ②The time distribution of global strong earthquakes with M ≥ 7.0 shows that the character of anomalous seismic quiescence-activity one year before the M_W9.0 earthquake and during its active period, the strong earthquakes formed a seismic belt striking in NWW direction. At the same time, there is a seismic gap formed by earthquakes of M ≥ 5.0 in the epicenter and its neighboring region. ③Two deep earthquakes of M ≥ 7.0 occurred in the west and in the east of the north boundary zone of the Australian plate half year ago. It is notable that one of them occurred in the Sumatra island where no deep earthquake with M ≥ 6.0 has occurred in the past thirty years. ④ The space distribution of moderate shocks occurring three days ago exhibited a NWW-strike seismic belt along the north boundary zone of the Australian plate. ⑤The activity of volcanoes distributed in the north boundary zone of the Australian plate had been strengthened in the past 4 years, especially several months before the occurrence of the M_W9.0 earthquake.
机译:研究了M_W9.0地震前不同时空域的地震活动特征。研究结果如下:①自1994年以来,澳大利亚板块北边界的深层地震活动明显增强,频率,幅度和深度都有所增加,特别是在地震深度的非均匀分布方面(即在500公里到689公里之间)。同时,苏门答腊岛及其附近地区M≥7.0的浅层地震也得到了明显加强,形成了长约1000 km,宽约300 km的加强区。 ②M≥7.0的全球强地震的时间分布表明,在M_W9.0地震发生的前一年及其活动期间,地震静止活动异常,强地震形成了向NWW方向撞击的地震带。同时,震中及其附近地区存在由M≥5.0地震形成的地震缝隙。 ③半年前,澳大利亚板块北边界带以西和以东发生了两次M≥7.0的深地震。值得注意的是,其中之一发生在苏门答腊岛,在过去的30年中,没有发生过M≥6.0的大地震。 ④三天前发生的中度震荡的空间分布沿澳大利亚板块北边界带出现了一次NWW地震带。 ⑤在过去的四年中,特别是在M_W9.0级地震发生前的几个月中,分布在澳大利亚板块北边界区域的火山活动得到了加强。

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