1923年关东地震的强震动地震学成果

Masayuki TAKEMURA
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引用次数: 0

摘要

1923年的关东地震(里氏7.9级)是日本最具破坏性的地震之一。针对这次地震进行了许多地震学和地震工程方面的研究。从1990年开始的15年里,对其震源过程和强地面运动的研究取得了特别大的进展。本文对这一时期的研究成果进行了综述。恢复了本吾的Ewing地震仪和Imamura地震仪的记录,并进行了模拟,以推测主震期间东京的长周期强地面运动。在这一时期,还发现了包括伊姆村地震仪记录在内的其他地震记录,这些记录完整地记录了几个台站的主震和余震的地面运动。这些地震记录有助于阐明主震的震源过程,主震有两个大的子事件,它们发生在距离断面上约40 km的地方,在最初的小破裂持续时间为3 ~ 5 s之后,时间间隔为10 ~ 15 s。主震复杂的断裂过程导致了近震源区强地面运动的区域变化,这是根据个人经验的描述估计出来的。余震序列也从这些地震记录中得到了澄清。在主震发生后3分钟和4.5分钟,又发生了2次M=7级余震,因此,关东地震发生的M=7级以上余震共有6次。关东地震的大余震次数明显大于其他M=8级俯冲事件。第一次大余震引起的第二次震动在JMA震级上对东京大都市区的地震烈度也估计为6级,尽管对个人经历的描述进行了分析,但与主震引起的第一次震动几乎相同。除上述研究外,在梳理了许多混乱的震害统计数据后,得到了这一时期关东地震的精确烈度分布。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
1923年関東地震に対する強震動地震学の成果
The 1923 Kanto earthquake (M=7.9) is one of the most destructive events in Japan. Many studies on seismology and earthquake engineering have been carried out for this earthquake. In one and half decade from 1990, investigations of its source process and strong ground motions had been especially advanced. This paper reviewed the results of the studies in this period. Records from Ewing seismoscope and Imamura seismograph at Hongo were restored and simulated to presume the long-period strong ground motion in Tokyo during the main shock. Other seismograms involving Imamura seismograph records which completely recorded ground motions from main shock and aftershocks at several stations were also revealed in this period. These seismograms were useful for elucidating the source process of the main shock having two big sub-events, whose locations were about 40 km distant on the fault plane, which occurred with time interval of 10 to 15 s after the initial small rupture duration of 3 to 5 s. This complex faulting process of the main shock caused the regional variations of strong ground motions in the near source region, which were estimated from the descriptions of personal experiences. The aftershock sequence was also clarified from these seismograms. Two M=7 class aftershocks were newly found to have occurred at 3 and 4.5 minutes after the main shock, so that total number of aftershocks with more than M=7 was six for the Kanto earthquake. The number of big aftershocks of the Kanto earthquake is meaningfully larger than the other M=8 class subduction events. The seismic intensity on the JMA scale due to the second shaking caused by the first big aftershock was also estimated to be 6 in Tokyo metropolitan area, though the analysis of the descriptions of personal experiences, which was almost the same as the first shaking by the main shock. Besides above studies, the precise seismic intensity distribution of the Kanto earthquake was obtained in this period, after raveling out many confused damage statistics data.
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