Three-dimensional topographic relief of the oceanic crust may control the occurrence of shallow very-low-frequency earthquakes in the Nankai Trough off Kumano
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DOI[10.1186/s40623-020-01204-3]のデータに遷移します
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- 資料種別
- 記事
- 著者・編者
- Kazuya ShiraishiYasuhiro YamadaMasaru Nakano
- 出版年月日等
- 2020-05-27
- 出版年（W3CDTF）
- 2020-05-27
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 72(72)
- 掲載巻
- 72(72)
- ISSN（掲載誌）
- 1880-5981
- ISSN-L（掲載誌）
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-020-01204-3
- 国立国会図書館永続的識別子
- info:ndljp/pid/11520526
- 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）
- 2020-08-03T12:00:21+09:00
- 保存日（W3CDTF）
- 2020-08-03
- 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/11467692
- 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
- コレクション : 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
- DOI
- 10.1186/s40623-020-01204-3
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報（URI）
- 参照
- The nature of the Pacific plate as subduction inputs to the northeastern Japan arc and its implication for subduction zone processesFrictional properties of the décollement in the shallow Nankai Trough: Constraints from friction experiments simulating in-situ conditions and implications for the seismogenic zoneA review of shallow slow earthquakes along the Nankai TroughHeterogeneous Sediment Input at the Nankai Trough Subduction Zone: Implications for Shallow Slow Earthquake LocalizationSpatial Patterns in Frictional Behavior of Sediments Along the Kumano Transect in the Nankai Trough南海トラフ沿いで発生する浅部スロー地震の特徴南海トラフにおける浅部スロー地震域の地震学的構造南海トラフにおける浅部スロー地震域の地質構造と摩擦特性Spatio-temporal distribution of shallow very-low-frequency earthquakes between December 2020 and January 2021 in Kumano-nada, Nankai subduction zone, detected by a permanent seafloor seismic networkDepth profile of frictional properties in the inner Nankai accretionary prism using cuttings from IODP Site C0002Evolution of the geological structure and mechanical properties due to the collision of multiple basement topographic highs in a forearc accretionary wedge : insights from numerical simulations
- 参照
- Dynamic deformation of the accretionary prism excites very low frequency earthquakesCharacteristics of a tsunamigenic megasplay fault in the Nankai TroughConnecting slow earthquakes to large earthquakesDistribution of stress state in the Nankai subduction zone, southwest Japan and a comparison with Japan TrenchMiddle Miocene swift migration of the TTT triple junction and rapid crustal growth in southwest Japan: A reviewSporadic low-velocity volumes spatially correlate with shallow very low frequency earthquake clustersEarthquakes and Tremor Linked to Seamount Subduction During Shallow Slow Slip at the Hikurangi Margin, New ZealandSlow slip near the trench at the Hikurangi subduction zone, New ZealandStructural Characteristics of the Nankai Trough Shallow Plate Boundary Inferred From Shallow Very Low Frequency EarthquakesThe slow earthquake spectrum in the Japan Trench illuminated by the S-net seafloor observatoriesInvited review paper: Fault creep caused by subduction of rough seafloor reliefThree-Dimensional Splay Fault Geometry and Implications for Tsunami GenerationDetailed structural image around splay‐fault branching in the Nankai subduction seismogenic zone: Results from a high‐density ocean bottom seismic surveyCrustal deformation dynamics and stress evolution during seamount subduction: High‐resolution 3‐D numerical modelingSubducted Seamount Imaged in the Rupture Zone of the 1946 Nankaido EarthquakeCrustal velocity field of southwest Japan: Subduction and arc‐arc collisionMechanical and hydrological effects of seamount subduction on megathrust stress and slipAn updated digital model of plate boundariesWeak Interplate Coupling by Seamounts and Repeating <i>M</i> ~ 7 EarthquakesBroad, weak regions of the Nankai Megathrust and implications for shallow coseismic slipTectonic Evolution of the Japanese Island Arc SystemSource mechanisms and tectonic significance of historical earthquakes along the nankai trough, JapanA large silent earthquake in the Guerrero seismic gap, MexicoSubducted seamount diverts shallow slow slip to the forearc of the northern Hikurangi subduction zone, New ZealandTsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slipMigrating tremor off southern Kyushu as evidence for slow slip of a shallow subduction interfaceA low-velocity zone with weak reflectivity along the Nankai subduction zoneSeismogenic Zone Structures Revealed by Improved 3‐D Seismic Images in the Nankai Trough off KumanoSpatial and temporal evolution of the megasplay fault in the Nankai TroughWaveform tomography imaging of a megasplay fault system in the seismogenic Nankai subduction zoneElevated pore pressure and anomalously low stress in regions of low frequency earthquakes along the Nankai Trough subduction megathrustShallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zoneRecurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrustSeismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on Integrated Ocean Drilling Program NanTro SEIZE coresA model for the motion of the Philippine Sea Plate consistent with NUVEL‐1 and geological dataConstruction of the DONET real-time seafloor observatory for earthquakes and tsunami monitoringDo subducting seamounts generate or stop large earthquakes?3-D seismic attributes using a semblance-based coherency algorithmTHERMOGENIC PETROLEUM POTENTIAL OF THE NANKAI SUBDUCTION ZONE, OFFSHORE SW JAPANEncyclopedic Dictionary of Applied GeophysicsExpedition 322 summaryDiverse slow slip behavior at the Hikurangi subduction margin, New ZealandWidely distributed thrust and strike-slip faults within subducting oceanic crust in the Nankai Trough off the Kii Peninsula, JapanA subducted oceanic ridge influencing the Nankai megathrust earthquake ruptureDistribution of very low frequency earthquakes in the Nankai accretionary prism influenced by a subducting-ridge3D beam prestack depth migration with examples from around the worldIntraoceanic thrusts in the Nankai Trough off the Kii Peninsula: Implications for intraplate earthquakesEpisodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent SlipSubducting seamounts control interplate coupling and seismic rupture in the 2014 Iquique earthquake areaSlow Earthquakes Coincident with Episodic Tremors and Slow Slip EventsPore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zoneLow‐frequency tremors associated with reverse faults in a shallow accretionary prismOrigin and evolution of a splay fault in the Nankai accretionary wedge
- 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
- 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Japan Link CenterCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 11520526