南大西洋・サウスサンドウィッチ諸島で2021年に発生した謎の津波地震の震源過程を解明

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2025-05-28 京都大学

京都大学の研究チームは、2021年にサウスサンドウィッチ諸島沖で発生したMw8.3〜8.5の津波地震の震源過程を詳細に解析しました。この地震は揺れに対して異常に大きな津波を伴う「津波地震」として注目され、解析により異なる性質を持つ4つの破壊エピソードから構成されていることが判明。特に第3エピソードのゆっくりとした断層破壊が第4の大規模すべりを誘発したことが明らかにされました。これらの知見は津波警報や被害軽減に貢献することが期待されます。

南大西洋・サウスサンドウィッチ諸島で2021年に発生した謎の津波地震の震源過程を解明
本研究の解析対象地域と解析結果

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2021年サウスサンドウィッチ諸島で発生した長周期地震津波の複雑な破砕進化 The complex rupture evolution of the long and slow, tsunamigenic 2021 South Sandwich Islands earthquake

Ryo Yamaguchi,Yuji Yagi,Ryo Okuwaki & Bogdan Enescu
Scientific Reports  Published:21 May 2025
DOI:https://doi.org/10.1038/s41598-025-02043-6

Abstract

On August 21, 2021, a large earthquake occurred in the South Sandwich subduction zone, and the associated tsunami was widely observed. To robustly analyse the detailed seismic source process of this long-source duration (over 200 s) event occurring in a convexly shaped subduction zone, we applied the Potency Density Tensor Inversion with a non-rectangular and non-planar source surface to the broadband teleseismic P-waves. This method allows us to suitably reduce the effect of the time-increasing uncertainty of the Green’s function and the effect of modelling errors related to the fault geometry. We found the slip vectors of the 400 km long rupture area rotate clockwise to the south, corresponding to the clockwise rotation of the trench strike. Our results reveal that the rupture propagated up-dip to the shallow region, then propagated to the south-southeast along the trench, and stagnated for about 30 s at around 130 km south-southeast from the epicentre. After the stagnation of the rupture front, the moment-rate gradually increased with time, although a clear rupture area could not be identified for about 45 s. Afterwards the rupture re-propagated south-southwest along the trench from the stagnation area. The slow rupture growth following the stagnation of the fast rupture triggered a new fast rupture, which led to the 2021 South Sandwich Islands earthquake having the typical characteristics of a tsunami earthquake, with a long rupture duration and a slow average rupture front velocity.

1702地球物理及び地球化学
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