Normal-faulting stress state associated with low differential stress in an overriding plate in northeast Japan prior to the 2011 Mw 9.0 Tohoku earthquake

• 資料種別: 記事
• タイトル: Normal-faulting stress state associated with low differential stress in an overriding plate in northeast Japan prior to the 2011 Mw 9.0 Tohoku earthquake
• 著者・編者: Makoto Otsubo; Ayumu Miyakawa; Kazutoshi Imanishi
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2018-03-26
• 出版年（W3CDTF）: 2018-03-26
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 70(51)
• 掲載巻: 70(51)
• 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/s40623-018-0813-9; https://doi.org/10.1186/s40623-018-0813-9
• 国立国会図書館永続的識別子: info:ndljp/pid/11067508; https://dl.ndl.go.jp/pid/11067508
• 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）: 2018-04-12T16:47:48+09:00
• 保存日（W3CDTF）: 2018-04-12
• 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/11067456; https://dl.ndl.go.jp/pid/11067456
• 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/s40623-018-0813-9; https://doi.org/10.1186/s40623-018-0813-9
• 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/11067508; https://dl.ndl.go.jp/pid/11067508; http://link.springer.com/article/10.1186/s40623-018-0813-9/fulltext.html; http://link.springer.com/content/pdf/10.1186/s40623-018-0813-9.pdf
• 参照: Crustal dynamics: unified understanding of geodynamic processes at different time and length scales; https://cir.nii.ac.jp/crid/1050564285813661696; Coseismic slickenlines record the emergence of multiple rupture fronts during a surface-breaking earthquake; https://cir.nii.ac.jp/crid/1360576118818604800; Surface rupture and characteristics of a fault associated with the 2011 and 2016 earthquakes in the southern Abukuma Mountains, northeastern Japan, triggered by the Tohoku-Oki earthquake; https://cir.nii.ac.jp/crid/2051714791998694528
• 参照: Imaging the source regions of normal faulting sequences induced by the 2011 M9.0 Tohoku‐Oki earthquake; https://cir.nii.ac.jp/crid/1360004230122138880; The 2011 Tohoku earthquake (Mw 9.0) sequence and subduction dynamics in Western Pacific and East Asia; https://cir.nii.ac.jp/crid/1360004232324606464; Stress before and after the 2011 great Tohoku‐oki earthquake and induced earthquakes in inland areas of eastern Japan; https://cir.nii.ac.jp/crid/1360004233288308864; Changes in seismic activity following the 2011 Tohoku-oki earthquake: Effects of pore fluid pressure; https://cir.nii.ac.jp/crid/1360283690892926848; Depth-dependent stress field in and around the Atotsugawa fault, central Japan, deduced from microearthquake focal mechanisms: Evidence for localized aseismic deformation in the downward extension of the fault; https://cir.nii.ac.jp/crid/1360285708263913856; New, improved version of generic mapping tools released; https://cir.nii.ac.jp/crid/1360292617909532032; Simultaneous Reactivation of Two, Subparallel, Inland Normal Faults during the Mw 6.6 11 April 2011 Iwaki Earthquake Triggered by the Mw 9.0 Tohoku-oki, Japan, Earthquake; https://cir.nii.ac.jp/crid/1360567188144044032; Temporal slip change based on curved slickenlines on fault scarps along Itozawa fault caused by 2011 Iwaki earthquake, northeast Japan; https://cir.nii.ac.jp/crid/1360848657453500544; Spatially heterogeneous stress field in the source area of the 2011 Mw 6.6 Fukushima-Hamadori earthquake, NE Japan, probably caused by static stress change; https://cir.nii.ac.jp/crid/1360848659520126464; Determination of stress from slip data: Faults and folds; https://cir.nii.ac.jp/crid/1360855570873587456; Structural Analysis of Coseismic Normal Fault Zones of the 2011 Mw 6.6 Fukushima Earthquake, Northeast Japan; https://cir.nii.ac.jp/crid/1360855571244284032; Effect of a change in the state of stress on the likelihood of inland fault failure during the Mw 6.6 Iwaki earthquake resulting from the Mw 9.0 2011 Tohoku earthquake, Japan; https://cir.nii.ac.jp/crid/1361137044482226560; Crustal extensional faulting triggered by the 2010 Chilean earthquake: The Pichilemu Seismic Sequence; https://cir.nii.ac.jp/crid/1361137044797096192; A stress inversion procedure for polyphase fault/slip data sets; https://cir.nii.ac.jp/crid/1361418520085007360; Coseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquake; https://cir.nii.ac.jp/crid/1361418520750308480; The 2011 Magnitude 9.0 Tohoku-Oki Earthquake: Mosaicking the Megathrust from Seconds to Centuries; https://cir.nii.ac.jp/crid/1361981469343259520; 3-D rotation of double-couple earthquake sources; https://cir.nii.ac.jp/crid/1361981470667329536; The Mechanics of Oblique Slip Faulting; https://cir.nii.ac.jp/crid/1362262943593336320; Computerized identification of stress tensors determined from heterogeneous fault-slip data by combining the multiple inverse method and k-means clustering; https://cir.nii.ac.jp/crid/1362262943836017792; An improved method for determining the regional stress tensor using earthquake focal mechanism data: Application to the San Fernando Earthquake Sequence; https://cir.nii.ac.jp/crid/1362262944326031360; Distances for the solutions of stress tensor inversion in relation to misfit angles that accompany the solutions; https://cir.nii.ac.jp/crid/1362544420416859904; The multiple inverse method applied to meso-scale faults in mid-Quaternary fore-arc sediments near the triple trench junction off central Japan; https://cir.nii.ac.jp/crid/1362825894995947904; Progressive fault triggering and fluid flow in aftershock domains: Examples from mineralized Archaean fault systems; https://cir.nii.ac.jp/crid/1363107370920254208; Geometry of Shearing Stress and Relation to Faulting; https://cir.nii.ac.jp/crid/1363388844618300288; Determination of stresses from heterogeneous focal mechanism data: An adaptation of the multiple inverse method; https://cir.nii.ac.jp/crid/1363670321261110016; Unusual shallow normal‐faulting earthquake sequence in compressional northeast Japan activated after the 2011 off the Pacific coast of Tohoku earthquake; https://cir.nii.ac.jp/crid/1363951795233402880; Implications of fault-valve behaviour for rupture nucleation and recurrence; https://cir.nii.ac.jp/crid/1363951795302132608; Spatial variations in stress within the 1987 Whittier Narrows, California, aftershock sequence: New techniques and results; https://cir.nii.ac.jp/crid/1364233268854656256; Outline of the 2011 off the Pacific coast of Tohoku Earthquake (Mw 9.0) : seismicity: foreshocks, mainshock, aftershocks, and induced activity; https://cir.nii.ac.jp/crid/2050588892138312576; Interplate fault slip along the Japan Trench before the occurrence of the 2011 off the Pacific coast of Tohoku Earthquake as inferred from GPS data; https://cir.nii.ac.jp/crid/2051996267021870080
• 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）: 11067508; http://id.ndl.go.jp/bib/11067508