{"title":"2021年宫城县地震的破裂运动学:日本海沟俯冲带高速体中的重复地震事件","authors":"Jiaqi Qian, Wenbo Zhang, Ao Zheng","doi":"10.1007/s00024-025-03673-7","DOIUrl":null,"url":null,"abstract":"<div><p>The 2021 Miyagi-Oki earthquakes (<i>M</i><sub>w</sub> 7.1 and <i>M</i><sub>w</sub> 6.8) occurred in rapid succession within the Japan Trench subduction zone, one of the most seismically active regions globally. To investigate the rupture processes and interactions between these events, we performed the joint inversions of strong-motion and teleseismic waveforms. The inversion results for the <i>M</i><sub>w</sub> 7.1 Miyagi-Oki earthquake reveal a bilateral rupture along a megathrust fault. A large asperity in the southern section of the seismogenic fault extends from deep portions to the top edge, with a maximum slip of 1.4 m. In contrast, the <i>M</i><sub>w</sub> 6.8 Miyagi-Oki earthquake exhibits a unilateral rupture with a peak slip of about 1.1 m. Aftershocks following both earthquakes generally occurred at shallower depths than the initial rupture, likely influenced by focal depth, fault geometry, and fluid migration. The recurrence of earthquakes in the Miyagi-Oki region reflects the periodic release of accumulated strain on high-velocity bodies due to interseismic locking and stress loading from nearby large earthquakes. Coulomb stress analysis suggests that the 2021 <i>M</i><sub>w</sub> 7.1 Fukushima-Oki earthquake may have triggered the subsequent 2021 <i>M</i><sub>w</sub> 7.1 Miyagi-Oki earthquake, with both events contributing to the <i>M</i><sub>w</sub> 6.8 Miyagi-Oki earthquake. These findings enhance our understanding of earthquake triggering mechanisms and provide key insights into future seismic hazards in the Japan Trench subduction zone.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"182 2","pages":"333 - 346"},"PeriodicalIF":1.9000,"publicationDate":"2025-02-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Rupture Kinematics of the 2021 Miyagi-Oki Earthquakes: Repeated Seismic Events in High-Velocity Bodies of the Japan Trench Subduction Zone\",\"authors\":\"Jiaqi Qian, Wenbo Zhang, Ao Zheng\",\"doi\":\"10.1007/s00024-025-03673-7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The 2021 Miyagi-Oki earthquakes (<i>M</i><sub>w</sub> 7.1 and <i>M</i><sub>w</sub> 6.8) occurred in rapid succession within the Japan Trench subduction zone, one of the most seismically active regions globally. To investigate the rupture processes and interactions between these events, we performed the joint inversions of strong-motion and teleseismic waveforms. The inversion results for the <i>M</i><sub>w</sub> 7.1 Miyagi-Oki earthquake reveal a bilateral rupture along a megathrust fault. A large asperity in the southern section of the seismogenic fault extends from deep portions to the top edge, with a maximum slip of 1.4 m. In contrast, the <i>M</i><sub>w</sub> 6.8 Miyagi-Oki earthquake exhibits a unilateral rupture with a peak slip of about 1.1 m. Aftershocks following both earthquakes generally occurred at shallower depths than the initial rupture, likely influenced by focal depth, fault geometry, and fluid migration. The recurrence of earthquakes in the Miyagi-Oki region reflects the periodic release of accumulated strain on high-velocity bodies due to interseismic locking and stress loading from nearby large earthquakes. Coulomb stress analysis suggests that the 2021 <i>M</i><sub>w</sub> 7.1 Fukushima-Oki earthquake may have triggered the subsequent 2021 <i>M</i><sub>w</sub> 7.1 Miyagi-Oki earthquake, with both events contributing to the <i>M</i><sub>w</sub> 6.8 Miyagi-Oki earthquake. These findings enhance our understanding of earthquake triggering mechanisms and provide key insights into future seismic hazards in the Japan Trench subduction zone.</p></div>\",\"PeriodicalId\":21078,\"journal\":{\"name\":\"pure and applied geophysics\",\"volume\":\"182 2\",\"pages\":\"333 - 346\"},\"PeriodicalIF\":1.9000,\"publicationDate\":\"2025-02-17\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"pure and applied geophysics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s00024-025-03673-7\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"pure and applied geophysics","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s00024-025-03673-7","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Rupture Kinematics of the 2021 Miyagi-Oki Earthquakes: Repeated Seismic Events in High-Velocity Bodies of the Japan Trench Subduction Zone
The 2021 Miyagi-Oki earthquakes (Mw 7.1 and Mw 6.8) occurred in rapid succession within the Japan Trench subduction zone, one of the most seismically active regions globally. To investigate the rupture processes and interactions between these events, we performed the joint inversions of strong-motion and teleseismic waveforms. The inversion results for the Mw 7.1 Miyagi-Oki earthquake reveal a bilateral rupture along a megathrust fault. A large asperity in the southern section of the seismogenic fault extends from deep portions to the top edge, with a maximum slip of 1.4 m. In contrast, the Mw 6.8 Miyagi-Oki earthquake exhibits a unilateral rupture with a peak slip of about 1.1 m. Aftershocks following both earthquakes generally occurred at shallower depths than the initial rupture, likely influenced by focal depth, fault geometry, and fluid migration. The recurrence of earthquakes in the Miyagi-Oki region reflects the periodic release of accumulated strain on high-velocity bodies due to interseismic locking and stress loading from nearby large earthquakes. Coulomb stress analysis suggests that the 2021 Mw 7.1 Fukushima-Oki earthquake may have triggered the subsequent 2021 Mw 7.1 Miyagi-Oki earthquake, with both events contributing to the Mw 6.8 Miyagi-Oki earthquake. These findings enhance our understanding of earthquake triggering mechanisms and provide key insights into future seismic hazards in the Japan Trench subduction zone.
期刊介绍:
pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys.
Long running journal, founded in 1939 as Geofisica pura e applicata
Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences
Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research
Coverage extends to research topics in oceanic sciences
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