地震の頻度分布と発生効率から見た大地震の切迫度~2016年熊本地震前後の活動への適用~

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2025-05-26 九州大学

九州大学の松本聡教授は、地震の「b値」と新たに提案した「効率」指標を組み合わせることで、大地震の発生位置を特定する手法を開発しました。「効率」は、地震のモーメントを用いて岩盤がどれだけ効果的に壊れているかを示す指標で、強い地震が発生しやすい領域の判別に有効です。この手法を2016年熊本地震前後の活動に適用し、本震の発生箇所を特定できることを実証。地震予測や防災対策への活用が期待されます。

地震の頻度分布と発生効率から見た大地震の切迫度~2016年熊本地震前後の活動への適用~
図1 熊本地震前の活動から見た、深さ10-20㎞のb値と臨界度活動指標分布

<関連情報>

地震モーメント効率と小地震の頻度-回数分布が示す大地震の近接性 LARGE earthquake proximity indicated by seismic moment efficiency and frequency-number distribution of small earthquakes

Satoshi Matsumoto
Scientific Reports  Published:19 May 2025
DOI:https://doi.org/10.1038/s41598-025-01595-x

Abstract

The size distribution of minor earthquakes, characterized by a power-law decay (b-value), sometimes indicates the hazard information of major earthquakes. Studies show that the b-value reflects the stress level and proximity of the fault failure condition. However, the mechanisms are difficult to determine. This study proposes an additional proximity indicator that is ratio of stacked seismic moment tensor to total moment release in a volume. The ratio indicates efficiency of inelastic strain due to seismic moment release by earthquakes, being close to the strength of the medium based on the Mohr diagram and Coulomb failure condition. We examined the b-value and efficiency variations in pre- and post-seismic activities of the 2016 Kumamoto earthquake sequence. The weighted b-value distribution based on efficiency captured the initiation point of the Kumamoto earthquake. Thus, utilizing both b-value and efficiency can improve earthquake alerts and disaster mitigation.

1702地球物理及び地球化学
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