Spatial variation in coda Q in the northeastern part of Niigata–Kobe Tectonic Zone, central Japan : implication of the cause of a high strain rate zone

• 資料種別: 記事
• タイトル: Spatial variation in coda Q in the northeastern part of Niigata–Kobe Tectonic Zone, central Japan : implication of the cause of a high strain rate zone
• 著者・編者: Masanobu Dojo; Yoshihiro Hiramatsu
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2017-06-05
• 出版年（W3CDTF）: 2017-06-05
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 69(76)
• 掲載巻: 69(76)
• 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/s40623-017-0663-x; https://doi.org/10.1186/s40623-017-0663-x
• 国立国会図書館永続的識別子: info:ndljp/pid/10369103; https://dl.ndl.go.jp/pid/10369103
• 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）: 2017-06-22T22:40:19+09:00
• 保存日（W3CDTF）: 2017-06-22
• 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）: http://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/10319651; https://dl.ndl.go.jp/pid/10319651
• 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/s40623-017-0663-x; https://doi.org/10.1186/s40623-017-0663-x
• 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/10369103; https://dl.ndl.go.jp/pid/10369103; http://link.springer.com/content/pdf/10.1186/s40623-017-0663-x.pdf; http://link.springer.com/article/10.1186/s40623-017-0663-x/fulltext.html
• 参照: Crustal dynamics: unified understanding of geodynamic processes at different time and length scales; https://cir.nii.ac.jp/crid/1050564285813661696; Temporal stability of coda Q in the northeastern part of an inland high strain rate zone, central Japan : implication of a persistent ductile deformation in the crust; https://cir.nii.ac.jp/crid/2051433317020892288
• 参照: Temporal change in shear velocity and polarization anisotropy related to the 2011 M9.0 Tohoku‐Oki earthquake examined using KiK‐net vertical array data; https://cir.nii.ac.jp/crid/1360002216709540480; Response of seismicity to static and dynamic stress changes induced by the 2011 <i>M</i>9.0 Tohoku‐Oki earthquake; https://cir.nii.ac.jp/crid/1360285705098984960; New, improved version of generic mapping tools released; https://cir.nii.ac.jp/crid/1360292617909532032; Spontaneous Rupture Propagation on a Non-planar Fault in 3-D Elastic Medium; https://cir.nii.ac.jp/crid/1360292621467787392; Spatial distribution of scattering loss and intrinsic absorption of short-period<i>S</i>waves in the lithosphere of Japan on the basis of the Multiple Lapse Time Window Analysis of Hi-net data; https://cir.nii.ac.jp/crid/1360565168144255488; Analysis of the seismic coda of local earthquakes as scattered waves; https://cir.nii.ac.jp/crid/1360574092883497728; Deep crustal structure along the Niigata-Kobe Tectonic Zone, Japan: Its origin and segmentation; https://cir.nii.ac.jp/crid/1360574096419106432; Scattering and attenuation of shear waves in the lithosphere; https://cir.nii.ac.jp/crid/1361137044779247104; Water-weakened lower crust and its role in the concentrated deformation in the Japanese Islands; https://cir.nii.ac.jp/crid/1361981469009516544; Three-dimensional P- and S-wave velocity structures beneath the Japan Islands obtained by high-density seismic stations by seismic tomography; https://cir.nii.ac.jp/crid/1362544420597522688; Temporal changes in coda <i>Q</i>⁻¹ and <i>b</i> value due to the static stress change associated with the 1995 Hyogo‐ken Nanbu earthquake; https://cir.nii.ac.jp/crid/1362544421005708672; Spatial and Temporal Variations in Coda Attenuation Associated with the 2011 Off the Pacific Coast of Tohoku, Japan (Mw 9) Earthquake; https://cir.nii.ac.jp/crid/1363107368637122048; Origin of coda waves: Source, attenuation, and scattering effects; https://cir.nii.ac.jp/crid/1363670320952940672; Geographical distribution of ³He/⁴He ratios in Japan: Implications for arc tectonics and incipient magmatism; https://cir.nii.ac.jp/crid/1364233268895034112; Relation between direct wave<i>Q</i>and coda<i>Q:</i>a numerical approach; https://cir.nii.ac.jp/crid/1364233270414625408; Origin of the concentrated deformation zone in the Japanese Islands and stress accumulation process of intraplate earthquakes; https://cir.nii.ac.jp/crid/1390001206513487360; High-resolution map of Coda Q in Japan and their interpretation by the brittle-ductile interaction hypothesis; https://cir.nii.ac.jp/crid/1390282681489262976; Anelastic properties beneath the Niigata-Kobe Tectonic Zone, Japan; https://cir.nii.ac.jp/crid/2050025942007323648; Spatial variation in coda Q and stressing rate around the Atotsugawa fault zone in a high strain rate zone, central Japan; https://cir.nii.ac.jp/crid/2050025942185011200; Spatial variation in coda Q around the Nobi fault zone, central Japan : relation to S-wave velocity and seismicity; https://cir.nii.ac.jp/crid/2050870367116803456; Spatial variation in shear wave splitting of the upper crust in the zone of inland high strain rate, central Japan; https://cir.nii.ac.jp/crid/2051433317068414336; Stress state in the upper crust around the source region of the 1891 Nobi earthquake through shear wave polarization anisotropy; https://cir.nii.ac.jp/crid/2051433317073003008
• 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）: 10369103; http://id.ndl.go.jp/bib/10369103