Repeated occurrence of surface-sediment remobilization along the landward slope of the Japan Trench by great earthquakes

• 資料種別: 記事
• タイトル: Repeated occurrence of surface-sediment remobilization along the landward slope of the Japan Trench by great earthquakes
• 著者・編者: Ken Ikehara; Kazuko Usami; Toshiya Kanamatsu
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2020-08-08
• 出版年（W3CDTF）: 2020-08-08
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 72(114)
• 掲載巻: 72(114)
• 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/s40623-020-01241-y; https://doi.org/10.1186/s40623-020-01241-y
• 国立国会図書館永続的識別子: info:ndljp/pid/11616199; https://dl.ndl.go.jp/pid/11616199
• コレクション（共通）: 障害者向け資料
• コレクション（障害者向け資料：レベル1）: テキストデータ
• 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; https://dl.ndl.go.jp/collections/B00035
• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2021-01-13T14:13:05+09:00
• 保存日（W3CDTF）: 2021-01-13
• 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（URI）: https://earth-planets-space.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/11467692; https://dl.ndl.go.jp/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; https://dl.ndl.go.jp

• 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/s40623-020-01241-y; https://doi.org/10.1186/s40623-020-01241-y
• 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）: http://id.ndl.go.jp/digimeta/11616199; https://dl.ndl.go.jp/pid/11616199; https://link.springer.com/content/pdf/10.1186/s40623-020-01241-y.pdf; https://link.springer.com/article/10.1186/s40623-020-01241-y/fulltext.html
• 参照: A Decade of Lessons Learned from the 2011 Tohoku‐Oki Earthquake; https://cir.nii.ac.jp/crid/1360009142423994240; Expedition 386 Preliminary Report: Japan Trench Paleoseismology; https://cir.nii.ac.jp/crid/1360017287039195264; Comparative single-cell genomics of Atribacterota JS1 in the Japan Trench hadal sedimentary biosphere; https://cir.nii.ac.jp/crid/1360021391875895424; Japan Trench event stratigraphy: First results from IODP giant piston coring in a deep-sea trench to advance subduction zone paleoseismology; https://cir.nii.ac.jp/crid/1360588381074168064; Thermogenic methane and hydrogen generation in subducted sediments of the Nankai Trough; https://cir.nii.ac.jp/crid/1360865815686076672; 現行堆積作用・堆積物研究の地質学への展開： https://cir.nii.ac.jp/crid/1390574181058303744; 地震動による海底表層堆積物の再懸濁・再移動とそれを起源としたイベント堆積物を用いた地震履歴研究; https://cir.nii.ac.jp/crid/1390578614162710400; X-ray fluorescence core scanning, magnetic signatures, and organic geochemistry analyses of Ryukyu Trench sediments : turbidites and hemipelagites; https://cir.nii.ac.jp/crid/2050025942148537600; How large peak ground acceleration by large earthquakes could generate turbidity currents along the slope of northern Japan Trench; https://cir.nii.ac.jp/crid/2050870367089657600
• 参照: Hadal disturbance in the Japan Trench as induced by the 2011 Tohoku-Oki Earthquake; https://cir.nii.ac.jp/crid/1050845762388079744; Tsunami-generated turbidity current of the 2011 Tohoku-Oki earthquake; https://cir.nii.ac.jp/crid/1050845762388223104; Documenting large earthquakes similar to the 2011 Tohoku-oki earthquake from sediments deposited in the Japan Trench over the past 1500 years; https://cir.nii.ac.jp/crid/1360002215916334976; Evidence for surface sediment remobilization by earthquakes in the Nankai forearc region from sedimentary records; https://cir.nii.ac.jp/crid/1360002218608972800; Dynamic process of turbidity generation triggered by the 2011 Tohoku‐Oki earthquake; https://cir.nii.ac.jp/crid/1360004233289850112; Unexpected biotic resilience on the Japanese seafloor caused by the 2011 Tōhoku-Oki tsunami; https://cir.nii.ac.jp/crid/1360004233527982848; Event Stratigraphy in a Hadal Oceanic Trench: The Japan Trench as Sedimentary Archive Recording Recurrent Giant Subduction Zone Earthquakes and Their Role in Organic Carbon Export to the Deep Sea; https://cir.nii.ac.jp/crid/1360005744245282688; Turbidite Sedimentation in the Nankai Trough as Interpreted from Magnetic Fabric, Grain Size, and Detrital Modal Analyses; https://cir.nii.ac.jp/crid/1360011142930490496; Orleansville Earthquake and Turbidity Currents; https://cir.nii.ac.jp/crid/1360011142931415040; Paleoseismicity of the Cascadia Subduction Zone: Evidence from turbidites off the Oregon‐Washington Margin; https://cir.nii.ac.jp/crid/1360011142932826240; Episodic subsidence and active deformation of the forearc slope along the Japan Trench near the epicenter of the 2011 Tohoku Earthquake; https://cir.nii.ac.jp/crid/1360011142933538432; Turbidity currents and submarine slumps, and the 1929 Grand Banks [Newfoundland] earthquake; https://cir.nii.ac.jp/crid/1360011142935774080; Ponded Sediments of the Mid-Atlantic Ridge between 22° and 23° North Latitude; https://cir.nii.ac.jp/crid/1360011142936493184; Earthquake Impact on Active Margins: Tracing Surficial Remobilization and Seismic Strengthening in a Slope Sedimentary Sequence; https://cir.nii.ac.jp/crid/1360011142937796224; Tectonic erosion at the front of the Japan Trench convergent margin; https://cir.nii.ac.jp/crid/1360011142939309184; The importance of site selection, sediment supply, and hydrodynamics: A case study of submarine paleoseismology on the northern Cascadia margin, Washington USA; https://cir.nii.ac.jp/crid/1360011142939375744; Megathrust earthquake drives drastic organic carbon supply to the hadal trench; https://cir.nii.ac.jp/crid/1360288691706411008; Open-ocean to trench turbidity-current flow in the Nankai Trough: Flow collapse and reflection; https://cir.nii.ac.jp/crid/1360292617907108096; Summary, Japan Trench Transect; https://cir.nii.ac.jp/crid/1360292617907201152; Rupture lengths and temporal history of significant earthquakes on the offshore and north coast segments of the Northern San Andreas Fault based on turbidite stratigraphy; https://cir.nii.ac.jp/crid/1360292617912775808; Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan; https://cir.nii.ac.jp/crid/1360292617916830848; Tectonic erosion along the Japan and Peru convergent margins; https://cir.nii.ac.jp/crid/1360292617917276928; Crustal earthquakes; https://cir.nii.ac.jp/crid/1360292617918041344; Spatial variability in sediment lithology and sedimentary processes along the Japan Trench: use of deep-sea turbidite records to reconstruct past large earthquakes; https://cir.nii.ac.jp/crid/1360565168562352768; Long-term monitoring of bottom environments of the continental slope off Otsuchi Bay, northeastern Japan; https://cir.nii.ac.jp/crid/1360567181335313408; Possible submarine tsunami deposits on the outer shelf of Sendai Bay, Japan resulting from the 2011 earthquake and tsunami off the Pacific coast of Tohoku; https://cir.nii.ac.jp/crid/1360567182306256640; Benthic foraminiferal evidence of deep-sea sediment transport by the 2011 Tohoku-oki earthquake and tsunami; https://cir.nii.ac.jp/crid/1360574092883408000; Seismoturbidite record as preserved at core sites at the Cascadia and Sumatra–Andaman subduction zones; https://cir.nii.ac.jp/crid/1360574092886626944; Geologically current plate motions; https://cir.nii.ac.jp/crid/1360574092887403392; Sequence of structures in fine-grained turbidites: Comparison of recent deep-sea and ancient flysch sediments; https://cir.nii.ac.jp/crid/1360574092890263808; Turbidity Currents, Submarine Landslides and the 2006 Pingtung Earthquake off SW Taiwan; https://cir.nii.ac.jp/crid/1360574092891623680; Supercycle in great earthquake recurrence along the Japan Trench over the last 4000 years; https://cir.nii.ac.jp/crid/1360574092892418176; High‐resolution chronology of sediment below <scp>CCD</scp> based on <scp>H</scp>olocene paleomagnetic secular variations in the <scp>T</scp>ohoku‐oki earthquake rupture zone; https://cir.nii.ac.jp/crid/1360846639281329792; Sedimentary organic matter contents and porewater chemistry at upper bathyal depths influenced by the 2011 off the Pacific coast of Tohoku Earthquake and tsunami; https://cir.nii.ac.jp/crid/1360846640328312576; Remobilization of surficial slope sediment triggered by the A.D. 2011 M_w9 Tohoku-Oki earthquake and tsunami along the Japan Trench; https://cir.nii.ac.jp/crid/1360846643404989824; Along‐arc structural variation of the plate boundary at the Japan Trench margin: Implication of interplate coupling; https://cir.nii.ac.jp/crid/1360855567862099968; Tectonically-triggered sediment and carbon export to the Hadal zone; https://cir.nii.ac.jp/crid/1360855567863047680; Lacustrine turbidites produced by surficial slope sediment remobilization: A mechanism for continuous and sensitive turbidite paleoseismic records; https://cir.nii.ac.jp/crid/1360855567864595328; Earthquakes drive large-scale submarine canyon development and sediment supply to deep-ocean basins; https://cir.nii.ac.jp/crid/1360855567864960384; Flow Behavior of Ponded Turbidity Currents; https://cir.nii.ac.jp/crid/1360855567867538176; Short term variability of Particle fluxes and its relation to variability in sea surface temperature and chlorophylla field detected by Ocean Color and Temperature Scanner (OCTS) off Sanriku, northwestern North Pacific in the spring of 1997; https://cir.nii.ac.jp/crid/1360855567869409024; Lacustrine turbidites as a tool for quantitative earthquake reconstruction: New evidence for a variable rupture mode in south central Chile; https://cir.nii.ac.jp/crid/1360855567870180224; Turbidite event history—Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone; https://cir.nii.ac.jp/crid/1360855567871518592; 深海底タービダイトの発生周期とその古地震学的意義; https://cir.nii.ac.jp/crid/1390001205220700672; 次の南海トラフ巨大地震に備えて 深海底タービダイトを用いた南海トラフ東部における地震発生間隔の推定; https://cir.nii.ac.jp/crid/1390282679207485568; 海底の地震・津波堆積物; https://cir.nii.ac.jp/crid/1390564238023962752; Possible climate preconditioning on submarine landslides along a convergent margin, Nankai Trough (NE Pacific); https://cir.nii.ac.jp/crid/2050307417098948992; Three-dimensional mapping and kinematic characterization of mass transport deposits along the outer Kumano Basin and Nankai accretionary wedge, southwest Japan; https://cir.nii.ac.jp/crid/2051714791995896576; Accumulation of an earthquake-induced extremely turbid layer in a terminal basin of the Nankai accretionary prism; https://cir.nii.ac.jp/crid/2051996267023636096
• 参照（URI）: https://cir.nii.ac.jp/crid/1370009142889602562
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
• 提供元機関・データベース: 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja
• 書誌ID（NDLBibID）: 11616199; http://id.ndl.go.jp/bib/11616199