Asperity distribution of the 1952 great Kamchatka earthquake and its relation to future earthquake potential in Kamchatka

被引:44
作者
Johnson, JM
Satake, K
机构
[1] Univ Tokyo, Earthquake Res Inst, Tokyo 113, Japan
[2] Geol Survey Japan, Seismotecton Sect, Tokyo, Japan
关键词
subduction zones; slip distribution; tsunamis;
D O I
10.1007/s000240050243
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The 1952 Kamchatka earthquake is among the largest earthquakes of this century, with an estimated magnitude of M-w = 9.0. We inverted tide gauge records from Japan, North America, the Aleutians, and Hawaii for the asperity distribution. The results show two areas of high slip. The average slip is over 3 m, giving a seismic moment estimate of 155 x 10(20) Nm, or M-w = 8.8. The 20th century seismicity of the 1952 rupture zone shows a strong correlation to the asperity distribution, which suggests that the large earthquakes (M > 7) are controlled by the locations of the asperities and that future large earthquakes will also recur in the asperity regions.
引用
收藏
页码:541 / 553
页数:13
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