How large peak ground acceleration by large earthquakes could generate turbidity currents along the slope of northern Japan Trench

• 資料種別: 記事
• タイトル: How large peak ground acceleration by large earthquakes could generate turbidity currents along the slope of northern Japan Trench
• 著者・編者: Ken Ikehara; Kazuko Usami; Toshiya Kanamatsu
• 出版事項: 日本 : Japan Geoscience Union
• 出版年月日等: 2023-02-27
• 出版年（W3CDTF）: 2023-02-27
• タイトル（掲載誌）: Progress in earth and planetary science
• 巻号年月日等（掲載誌）: 10(8)
• 掲載巻: 10(8)
• 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/s40645-023-00540-8; https://doi.org/10.1186/s40645-023-00540-8
• 国立国会図書館永続的識別子: info:ndljp/pid/12998723; https://dl.ndl.go.jp/pid/12998723
• 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）: 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（URI）: https://progearthplanetsci.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/12998715; https://dl.ndl.go.jp/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; 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/s40645-023-00540-8; https://doi.org/10.1186/s40645-023-00540-8
• 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/12998723; https://dl.ndl.go.jp/pid/12998723; https://link.springer.com/content/pdf/10.1186/s40645-023-00540-8.pdf; https://link.springer.com/article/10.1186/s40645-023-00540-8/fulltext.html
• 参照: Development of an offshore ground motion prediction equation for peak ground acceleration considering path effects based on S-net data; https://cir.nii.ac.jp/crid/1360025033656125184; 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; Submarine paleoseismology in the Japan Trench of northeastern Japan : turbidite stratigraphy and sedimentology using paleomagnetic and rock magnetic analyses; https://cir.nii.ac.jp/crid/2050307417136238208
• 参照: Hadal disturbance in the Japan Trench as induced by the 2011 Tohoku-Oki Earthquake; https://cir.nii.ac.jp/crid/1050845762388079744; 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; Paleoseismicity of the Cascadia Subduction Zone: Evidence from turbidites off the Oregon‐Washington Margin; https://cir.nii.ac.jp/crid/1360011142932826240; Turbidity currents and submarine slumps, and the 1929 Grand Banks [Newfoundland] earthquake; https://cir.nii.ac.jp/crid/1360011142935774080; 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 sequence of events around the epicentre of the 1929 Grand Banks earthquake: initiation of debris flows and turbidity current inferred from sidescan sonar; https://cir.nii.ac.jp/crid/1360011144922592384; A review of the rupture characteristics of the 2011 Tohoku-oki Mw 9.1 earthquake; https://cir.nii.ac.jp/crid/1360011146521954688; Deciphering hemipelagites from homogenites through anisotropy of magnetic susceptibility. Paleoseismic implications (Sea of Marmara and Gulf of Corinth); https://cir.nii.ac.jp/crid/1360013170332052480; Regional variability of slope stability: application to the Eel margin, California; https://cir.nii.ac.jp/crid/1360013172593736064; What controls the remobilization and deformation of surficial sediment by seismic shaking? Linking lacustrine slope stratigraphy to great earthquakes in South–Central Chile; https://cir.nii.ac.jp/crid/1360016869781588480; Geological and historical evidence of irregular recurrent earthquakes in Japan; https://cir.nii.ac.jp/crid/1360283692753624448; Submarine Slope Response to Earthquake Shaking Within Western Sagami Bay, Central Japan; https://cir.nii.ac.jp/crid/1360285705812745984; 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; Crustal earthquakes; https://cir.nii.ac.jp/crid/1360292617918041344; Physical and chemical associations of radionuclides and trace metals in estuarine sediments: an example from Poole Harbour, Southern England; https://cir.nii.ac.jp/crid/1360292620687609344; Characteristics and distribution of the event deposits induced by the 2011 Tohoku-oki earthquake and tsunami offshore of Sanriku and Sendai, Japan; https://cir.nii.ac.jp/crid/1360294646700981760; Event-dominated transport, provenance, and burial of organic carbon in the Japan Trench; https://cir.nii.ac.jp/crid/1360294647195629568; Quantifying the role of sandy–silty sediments in generating slope failures during earthquakes: example from the Algerian margin; https://cir.nii.ac.jp/crid/1360298759929346048; Sliding and regional slope stability in active margins: North Aegean Trough (Mediterranean); https://cir.nii.ac.jp/crid/1360298759930008576; Different depths of near-trench slips of the 1896 Sanriku and 2011 Tohoku earthquakes; https://cir.nii.ac.jp/crid/1360567186805261952; A 6600 year earthquake history in the region of the 2004 Sumatra-Andaman subduction zone earthquake; https://cir.nii.ac.jp/crid/1360574092885715968; 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; Seismological evidence for a lithospheric normal faulting — the Sanriku earthquake of 1933; https://cir.nii.ac.jp/crid/1360574092891912704; Supercycle in great earthquake recurrence along the Japan Trench over the last 4000 years; https://cir.nii.ac.jp/crid/1360574092892418176; The use of microstructures for discriminating turbiditic and hemipelagic muds and mudstones; https://cir.nii.ac.jp/crid/1360574093776307968; A review of the 2011 Tohoku-Oki earthquake (Mw 9.0): Large-scale rupture across heterogeneous plate coupling; https://cir.nii.ac.jp/crid/1360574095879520256; 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; 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; Flow path of the 1993 Hokkaido-Nansei-oki earthquake seismoturbidite, southern margin of the Japan sea north basin, inferred from anisotropy of magnetic susceptibility; https://cir.nii.ac.jp/crid/1360855569498752640; “Late Quaternary lacustrine paleo-seismic archives in north-western Alps: Examples of earthquake-origin assessment of sedimentary disturbances”; https://cir.nii.ac.jp/crid/1360855569615513728; Quantifying subaqueous slope stability during seismic shaking: Lake Lucerne as model for ocean margins; https://cir.nii.ac.jp/crid/1360855569983423104; High-resolution investigation of event driven sedimentation: Northeastern Gulf of Mexico; https://cir.nii.ac.jp/crid/1360857596548223104; Determination of photon self-absorption corrections for soil samples; https://cir.nii.ac.jp/crid/1360857597945284864; Sediments of Lake Vens (SW European Alps, France) record large-magnitude earthquake events; https://cir.nii.ac.jp/crid/1360861714567238784; Recent deposition of 90Sr and 137Cs observed in Tsukuba; https://cir.nii.ac.jp/crid/1361137043713918336; Magnetic anisotropy of rocks and its application in geology and geophysics; https://cir.nii.ac.jp/crid/1361137045203559936; Magnetic anisotropy and fabric of some foliated rocks from S.E. Australia; https://cir.nii.ac.jp/crid/1361418520912398464; Analysis of the 50-year records of the atmospheric deposition of long-lived radionuclides in Japan; https://cir.nii.ac.jp/crid/1361981468351471744; Paleoseismicity along the southern Kuril Trench deduced from submarine-fan turbidites; https://cir.nii.ac.jp/crid/1362262944450966272; Submarine paleoseismology of the northern Hikurangi subduction margin of New Zealand as deduced from Turbidite record since 16 ka; https://cir.nii.ac.jp/crid/1363107368521929728; 210Pb and 137Cs in sediments from Sagami Bay, Japan: sedimentation rates and inventories; https://cir.nii.ac.jp/crid/1363951796147689344; 断層タイプ及び地盤条件を考慮した最大加速度・最大速度の距離減衰式; https://cir.nii.ac.jp/crid/1390001205637384576; 1993年北海道南西沖地震の地震性タービダイトの堆積機構; https://cir.nii.ac.jp/crid/1390001206496771840; 1961年から1980年までの核実験に由来するSr-90,Cs-137とPu-239,240の年間降下量:簡単なモデルによる解析; https://cir.nii.ac.jp/crid/1390001206505008768; 三陸沖における再来大地震の震源過程の比較研究; https://cir.nii.ac.jp/crid/1390282679282413312; Subduction zone guided wave and the heterogeneity structure of the subducted plate: intensity anomalies in northern Japan; https://cir.nii.ac.jp/crid/1571135651469102080; Source process of the 2011 off the Pacific coast of Tohoku Earthquake with the combination of teleseismic and strong motion data; https://cir.nii.ac.jp/crid/2051714792045157120; Repeated occurrence of surface-sediment remobilization along the landward slope of the Japan Trench by great earthquakes; https://cir.nii.ac.jp/crid/2051996266981877376
• 参照（URI）: https://cir.nii.ac.jp/crid/1370580232387913474
• 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）: 12998723; http://id.ndl.go.jp/bib/12998723