A review on slow earthquakes in the Japan Trench
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- 資料種別
- 記事
- 著者・編者
- Tomoaki NishikawaSatoshi IdeTakuya Nishimura
- 出版年月日等
- 2023-01-03
- 出版年（W3CDTF）
- 2023-01-03
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 10(1)
- 掲載巻
- 10(1)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-022-00528-w
- 国立国会図書館永続的識別子
- info:ndljp/pid/12998716
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2023-09-27T14:40:47+09:00
- 保存日（W3CDTF）
- 2023-04-11
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/12998715
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- Slow earthquakes are episodic slow fault slips. They form a fundamental component of interplate deformation processes, along with fast, regular earthquakes. Recent seismological and geodetic observations have revealed detailed slow earthquake activity along the Japan Trench—the subduction zone where the March 11, 2011, moment magnitude (Mw) 9.0 Tohoku-Oki earthquake occurred. In this paper, we review observational, experimental, and simulation studies on slow earthquakes along the Japan Trench and their research history. By compiling the observations of slow earthquakes (e.g., tectonic tremors, very-low-frequency earthquakes, and slow slip events) and related fault slip phenomena (e.g., small repeating earthquakes, earthquake swarms, and foreshocks of large interplate earthquakes), we present an integrated slow earthquake distribution along the Japan Trench. Slow and megathrust earthquakes are spatially complementary in distribution, and slow earthquakes sometimes trigger fast earthquakes in their vicinities. An approximately 200-km-long along-strike gap of seismic slow earthquakes (i.e., tectonic tremors and very-low-frequency earthquakes) corresponds with the huge interplate locked zone of the central Japan Trench. The Mw 9.0 Tohoku-Oki earthquake ruptured this locked zone, but the rupture terminated without propagating deep into the slow-earthquake-genic regions in the northern and southern Japan Trench. Slow earthquakes are involved in both the rupture initiation and termination processes of megathrust earthquakes in the Japan Trench. We then compared the integrated slow earthquake distribution with the crustal structure of the Japan Trench (e.g., interplate sedimentary units, subducting seamounts, petit-spot volcanoes, horst and graben structures, residual gravity, seismic velocity structure, and plate boundary reflection intensity) and described the geological environment of the slow-earthquake-genic regions (e.g., water sources, pressure–temperature conditions, and metamorphism). The integrated slow earthquake distribution enabled us to comprehensively discuss the role of slow earthquakes in the occurrence process of the Tohoku-Oki earthquake. The correspondences of the slow earthquake distribution with the crustal structure and geological environment provide insights into the slow-earthquake-genesis in the Japan Trench and imply that highly overpressured fluids are key to understanding the complex slow earthquake distribution. Furthermore, we propose that detailed monitoring of slow earthquake activity can improve the forecasts of interplate seismicity along the Japan Trench.
- DOI
- 10.1186/s40645-022-00528-w
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- © The Author(s) 2022This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder.
- 関連情報（URI）
- 参照
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- 参照
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earthquakes, JapanA Lack of Dynamic Triggering of Slow Slip and Tremor Indicates That the Shallow Cascadia Megathrust Offshore Vancouver Island Is Likely LockedSilent fault slip following an interplate thrust earthquake at the Japan TrenchThermal and metamorphic environment of subduction zone episodic tremor and slipPeriodic Pulsing of Characteristic Microearthquakes on the San Andreas FaultDiscrimination of a preparatory stage leading to <i>M</i>7 characteristic earthquakes off Ibaraki Prefecture, JapanScaling law of seismic spectrumSeismicity variations associated with aseismic transients in Guerrero, Mexico, 1995–2006Mechanism of deep low frequency earthquakes: Further evidence that deep non‐volcanic tremor is generated by shear slip on the plate interfaceAn integrated perspective of the continuum between earthquakes and slow-slip phenomenaSediment effect on tsunami generation of the 1896 Sanriku Tsunami EarthquakeTidal triggering of earthquakes prior to the 2011 Tohoku‐Oki earthquake (<i>M</i><sub><i>w</i></sub> 9.1)Earthquakes and friction lawsAlong-dip variation of teleseismic short-period radiation from the 11 March 2011 Tohoku earthquake (M<sub>w</sub>9.0)Detection and characterization of transient forcing episodes affecting earthquake activity in the Aleutian Arc systemTectonic tremor along the northern Hikurangi Margin, New Zealand, between 2010 and 2015Source parameters of a M4.8 and its accompanying repeating earthquakes off Kamaishi, NE Japan: Implications for the hierarchical structure of asperities and earthquake cycleThe 1992 Nicaragua earthquake: a slow tsunami earthquake associated with subducted sedimentsDynamic modeling of slow earthquakes based on thermoporoelastic effects and inelastic generation of poresSubducted oceanic relief locks the shallow megathrust in central EcuadorEarthquake Initiation From Laboratory Observations and Implications for ForeshocksGeneric dependence of the frequency‐size distribution of earthquakes on depth and 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zoneA Silent Slip Event on the Deeper Cascadia Subduction InterfaceModeling fast and slow earthquakes at various scales2011年東北地方太平洋沖地震の震源過程1989年12月東京湾サイレント・アースクェイクの可能性The 1992 Sanriku-Oki, Japan, Ultra-Slow Earthquake.Co- and post-seismic slip associated with the 2005 Miyagi-oki earthquake (M7.2) as inferred from GPS dataGeodetic and seismic signatures of episodic tremor and slip in the northern Cascadia subduction zoneVery low frequency earthquakes excited by the 2004 off Kii peninsula earthquakes: a dynamic deformation process in the large accretionary prismSource process of the recurrent Tokachi-oki earthquake on September 26, inferred from teleseismic body wavesRepeating earthquakes and quasi-static slip on the plate boundary east off northern Honshu, Japan沈み込み帯におけるプレート境界面の不均質と地震活動沈み込み帯での水の循環様式(＜特集＞日本火山学会60周年「火山学の最新動向と今後の展望」)Petit-spot volcanism: A new type of volcanic zone discovered near a trenchThe centenary of the Omori formula for a decay of aftershock activityRepeating short- 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long-term slow slip event from 1996 to 1997 in the Kii Channel, JapanAmbient tectonic tremors in Manawatu, Cape Turnagain, Marlborough, and Puysegur, New ZealandDetection of deep low-frequency earthquakes in the Nankai subduction zone over 11 years using a matched filter techniqueCo- and postseismic slip behaviors extracted from decadal seafloor geodesy after the 2011 Tohoku-oki earthquakeA convolutional neural network-based classification of local earthquakes and tectonic tremors in Sanriku-oki, Japan, using S-net dataFocal mechanism and slip history of the 2011 Mw 9.1 off the Pacific coast of Tohoku Earthquake, constrained with teleseismic body and surface wavesFrictional and structural controls of seismic super-cycles at the Japan trenchImprovement on spatial resolution of a coseismic slip distribution using postseismic geodetic data through a viscoelastic inversionSpatiotemporal functional modeling of postseismic deformations after the 2011 Tohoku-Oki earthquakeCMT inversion for small-to-moderate earthquakes applying to dense short-period OBS array at off Ibaraki regionStatistic analysis of swarm activities around the Boso Peninsula, Japan : slow slip events beneath Tokyo Bay？Coupling coefficient, hierarchical structure, and earthquake cycle for the source area of the 2011 off the Pacific coast of Tohoku earthquake inferred from small repeating earthquake dataDetection of repeating earthquakes and their application in characterizing slow fault slipCatalog of small repeating earthquakes for the Japanese IslandsSeismicity distribution in the Tonankai and Nankai seismogenic zones and its spatiotemporal relationship with interplate coupling and slow earthquakesRegional and global variations in the temporal clustering of tectonic tremor activity
- 参照（URI）
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 12998716