Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescence

Abstract In subduction zones, slow slip events (SSEs) have been observed in the portion deeper than the downdip edge of seismogenic zone. However, since it is far offshore from geodetic networks on land, shallow SSEs near the trench axis are hardly observed. Despite of less quantitative than seafloo...

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Main Author: Kei Katsumata
Format: Article
Language:English
Published: SpringerOpen 2023-09-01
Series:Geoscience Letters
Subjects:
Online Access:https://doi.org/10.1186/s40562-023-00297-4
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author Kei Katsumata
author_facet Kei Katsumata
author_sort Kei Katsumata
collection DOAJ
description Abstract In subduction zones, slow slip events (SSEs) have been observed in the portion deeper than the downdip edge of seismogenic zone. However, since it is far offshore from geodetic networks on land, shallow SSEs near the trench axis are hardly observed. Despite of less quantitative than seafloor geodetic observations, a method for inferring the shallow SSEs based on seismic quiescence was presented in this study. Unusual decrease in occurrence rate of M ≥ 5.0 earthquakes was found in the southwestern Kurile Islands. The occurrence rate was ∼1.3 events/year between 1977 and around 2004 and no earthquake was observed during 16 years after 2004. The spatial pattern of the seismic quiescence can be explained qualitatively by the Coulomb failure stress change due to shallow SSE and its fault plane is on the upper boundary of the subducting Pacific plate in the focal area of the 1975 tsunami earthquake.
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spelling doaj.art-dcbdc57c30814399b3801c25fa46894d2023-11-20T09:37:47ZengSpringerOpenGeoscience Letters2196-40922023-09-0110111010.1186/s40562-023-00297-4Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescenceKei Katsumata0Institute of Seismology and Volcanology, Faculty of Science, Hokkaido UniversityAbstract In subduction zones, slow slip events (SSEs) have been observed in the portion deeper than the downdip edge of seismogenic zone. However, since it is far offshore from geodetic networks on land, shallow SSEs near the trench axis are hardly observed. Despite of less quantitative than seafloor geodetic observations, a method for inferring the shallow SSEs based on seismic quiescence was presented in this study. Unusual decrease in occurrence rate of M ≥ 5.0 earthquakes was found in the southwestern Kurile Islands. The occurrence rate was ∼1.3 events/year between 1977 and around 2004 and no earthquake was observed during 16 years after 2004. The spatial pattern of the seismic quiescence can be explained qualitatively by the Coulomb failure stress change due to shallow SSE and its fault plane is on the upper boundary of the subducting Pacific plate in the focal area of the 1975 tsunami earthquake.https://doi.org/10.1186/s40562-023-00297-4Seismic quiescenceSlow slip eventKurile IslandsTsunami earthquake
spellingShingle Kei Katsumata
Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescence
Geoscience Letters
Seismic quiescence
Slow slip event
Kurile Islands
Tsunami earthquake
title Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescence
title_full Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescence
title_fullStr Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescence
title_full_unstemmed Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescence
title_short Slow slip event in the focal area of the 1975 Kurile tsunami earthquake inferred from unusual long-term seismic quiescence
title_sort slow slip event in the focal area of the 1975 kurile tsunami earthquake inferred from unusual long term seismic quiescence
topic Seismic quiescence
Slow slip event
Kurile Islands
Tsunami earthquake
url https://doi.org/10.1186/s40562-023-00297-4
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