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Tidal triggering of earthquakes in Japan related to the regional tectonic stress

机译:与区域构造应力有关的日本地震的潮汐触发

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摘要

We observe a correlation between the Earth tide and earthquake occurrence that is closely related to the regional tectonic stress. We investigate the direction of the tidal compressional stress using shallow earthquakes occurring in 100 subregions of Japan for nearly five years. The azimuthal distribution of the compressional stress obtained for the observed earthquake data is compared with that synthesized for random earthquake occurrence. Statistical analysis confirms a significant difference between the observed and random catalogs for 13 subregions, which include the areas where unusual seismic activities took place recently, and where the possibility of future large earthquakes has been argued. For these subregions, earthquakes preferentially occur when the tidal compressional stress is near the dominant direction of P-axes of focal mechanisms obtained in the corresponding subregions. This suggests that the tidal stress may encourage earthquake occurrence when it acts in the direction to increase the regional tectonic stress.
机译:我们观察到地潮和地震发生之间的相关性与区域构造应力密切相关。我们使用近100年在日本100个次区域发生的浅层地震调查了潮汐压应力的方向。将观察到的地震数据获得的压应力的方位角分布与随机地震发生时合成的压应力的方位角分布进行比较。统计分析证实,在13个子区域的观测目录和随机目录之间存在显着差异,其中包括最近发生过异常地震活动的地区以及争论未来可能发生大地震的地区。对于这些子区域,当潮汐压缩应力接近在相应子区域中获得的震源机制的P轴的主导方向时,地震优先发生。这表明,潮汐应力作用于增加区域构造应力的方向时,可能会促进地震的发生。

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