Anelastic properties beneath the Niigata-Kobe Tectonic Zone, Japan

• 資料種別: 記事
• タイトル: Anelastic properties beneath the Niigata-Kobe Tectonic Zone, Japan
• 著者・編者: Junichi Nakajima; Toru Matsuzawa
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2017-02-22
• 出版年（W3CDTF）: 2017-02-22
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 69(33)
• 掲載巻: 69(33)
• 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/s40623-017-0619-1; https://doi.org/10.1186/s40623-017-0619-1
• 国立国会図書館永続的識別子: info:ndljp/pid/10319684; https://dl.ndl.go.jp/pid/10319684
• 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）: 2017-04-04T20:19:14+09:00
• 保存日（W3CDTF）: 2017-03-24
• 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/s40623-017-0619-1; https://doi.org/10.1186/s40623-017-0619-1
• オンライン閲覧公開範囲: インターネット公開
• 関連情報: Anelastic properties beneath the Niigata-Kobe Tectonic Zone, Japan; https://cir.nii.ac.jp/crid/2120589364471921280
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/10319684; https://dl.ndl.go.jp/pid/10319684; http://link.springer.com/content/pdf/10.1186/s40623-017-0619-1.pdf; http://link.springer.com/article/10.1186/s40623-017-0619-1/fulltext.html
• 参照: Crustal dynamics: unified understanding of geodynamic processes at different time and length scales; https://cir.nii.ac.jp/crid/1050564285813661696; Spatiotemporal changes in the strain field in the Niigata–Kobe Tectonic Zone: long-term analysis using GNSS time series data; https://cir.nii.ac.jp/crid/1050585172435286656; High-resolution three-dimensional azimuthal velocity anisotropy of S-waves in southern-central Japan, based on ambient noise tomography; https://cir.nii.ac.jp/crid/1360021391865419392; High-Resolution Three-dimensional Azimuthal Velocity Anisotropy of S-waves in southwest Japan, based on Ambient Noise Tomography; https://cir.nii.ac.jp/crid/1360022307170983936; Generative Adversarial Networks-Based Ground-Motion Model for Crustal Earthquakes in Japan Considering Detailed Site Conditions; https://cir.nii.ac.jp/crid/1360588380604428288; Detection of temporal change in near-source attenuation during intense fluid-driven seismicity following the 2011 Tohoku-Oki earthquake; https://cir.nii.ac.jp/crid/1360853567539472768; 地殻流体の起源・分布と変動現象; https://cir.nii.ac.jp/crid/1390001277392720384; 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; https://cir.nii.ac.jp/crid/2050588891962948096; 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: Three-dimensional seismic velocity structure and configuration of the Philippine Sea slab in southwestern Japan estimated by double-difference tomography; https://cir.nii.ac.jp/crid/1050001202746187904; Seismotectonics beneath the Tokyo metropolitan area, Japan: Effect of slab-slab contact and overlap on seismicity; https://cir.nii.ac.jp/crid/1050282677707608576; Seismic attenuation tomography of the Southwest Japan arc: new insight into subduction dynamics; https://cir.nii.ac.jp/crid/1360004234589961856; Plate convergence and long‐term crustal deformation in central Japan; https://cir.nii.ac.jp/crid/1360011142939448064; Imaging P and S attenuation in the termination region of the Hikurangi subduction zone, New Zealand; https://cir.nii.ac.jp/crid/1360011146038564736; Continuous GPS Array and Present-day Crustal Deformation of Japan; https://cir.nii.ac.jp/crid/1360013170949096064; Lateral variation of the cutoff depth of shallow earthquakes beneath the Japan Islands and its implications for seismogenesis; https://cir.nii.ac.jp/crid/1360283691152024448; Seismic attenuation beneath northeastern Japan: Constraints on mantle dynamics and arc magmatism; https://cir.nii.ac.jp/crid/1360285704777524736; Northern California Seismic Attenuation: 3D<i>Q</i>_<i>P</i>and<i>Q</i>_<i>S</i>Models; https://cir.nii.ac.jp/crid/1360292619762191360; Grainsize evolution in ductile shear zones: Implications for strain localization and the strength of the lithosphere; https://cir.nii.ac.jp/crid/1360292620863607168; 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; Grain‐size‐sensitive seismic wave attenuation in polycrystalline olivine; https://cir.nii.ac.jp/crid/1360574095347102336; Deep crustal structure along the Niigata-Kobe Tectonic Zone, Japan: Its origin and segmentation; https://cir.nii.ac.jp/crid/1360574096419106432; Slab‐derived fluids, fore‐arc hydration, and sub‐arc magmatism beneath Kyushu, Japan; https://cir.nii.ac.jp/crid/1360848654733823104; Double-planed structure of the deep seismic zone in the northeastern Japan arc; https://cir.nii.ac.jp/crid/1361418520735518080; Seismic attenuation and mantle wedge temperatures in the Alaska subduction zone; https://cir.nii.ac.jp/crid/1361699995992117632; P wave attenuation structure in the fault area of the 1995 Kobe earthquake; https://cir.nii.ac.jp/crid/1361699996220461440; Water-weakened lower crust and its role in the concentrated deformation in the Japanese Islands; https://cir.nii.ac.jp/crid/1361981469009516544; Seismic velocity structure of the crust beneath the Japan Islands; https://cir.nii.ac.jp/crid/1361981469072388736; The relationship between Late Cenozoic tectonic events and stress field and basin development in northeast Japan; https://cir.nii.ac.jp/crid/1361981471106492544; Seismic velocities in mantle minerals and the mineralogy of the upper mantle; https://cir.nii.ac.jp/crid/1362262945427081728; Tectonic stress and the spectra of seismic shear waves from earthquakes; https://cir.nii.ac.jp/crid/1362544420349513344; Deep structure of the northeastern Japan arc and its implications for crustal deformation and shallow seismic activity; https://cir.nii.ac.jp/crid/1363107368867931008; Strain accumulation process around the Atotsugawa fault system in the Niigata-Kobe Tectonic Zone, central Japan; https://cir.nii.ac.jp/crid/1363670320220357120; Tomographic imaging of <i>P</i> and <i>S</i> wave velocity structure beneath northeastern Japan; https://cir.nii.ac.jp/crid/1363670320746013056; Source parameters of a M4.8 and its accompanying repeating earthquakes off Kamaishi, NE Japan: Implications for the hierarchical structure of asperities and earthquake cycle; https://cir.nii.ac.jp/crid/1363951794626339328; Implications of fault-valve behaviour for rupture nucleation and recurrence; https://cir.nii.ac.jp/crid/1363951795302132608; Attenuation of seismic waves in dry and saturated rocks; I, Laboratory measurements; https://cir.nii.ac.jp/crid/1364233268626358784; Geothermal gradient and heat flow data in and around Japan (I): apprasial of heat flow from geothermal gradient data; https://cir.nii.ac.jp/crid/1390001206512574208; Mid-crustal electrical conductors and their correlations to seismicity and deformation at Itoigawa-Shizuoka Tectonic Line; https://cir.nii.ac.jp/crid/1390001206512576512; Origin of the concentrated deformation zone in the Japanese Islands and stress accumulation process of intraplate earthquakes; https://cir.nii.ac.jp/crid/1390001206513487360; Dislocation model for strain accumulation in a plate collision zone; https://cir.nii.ac.jp/crid/1390001206514075264; Heterogeneous crustal deformation along the central-northern Itoigawa-Shizuoka Tectonic Line Fault system, Central Japan; https://cir.nii.ac.jp/crid/1390001206514148992; 新潟－神戸ひずみ集中帯を横断する測地観測による越後平野周辺の地殻変動; https://cir.nii.ac.jp/crid/1390282679279991424; High-resolution map of Coda Q in Japan and their interpretation by the brittle-ductile interaction hypothesis; https://cir.nii.ac.jp/crid/1390282681489262976; Geochemical evidence for enhanced fluid flux due to overlapping subducting plates; https://cir.nii.ac.jp/crid/1572824501316275200; 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; Pore pressure distribution in the focal region of the 2008 M7.2 Iwate-Miyagi Nairiku earthquake; https://cir.nii.ac.jp/crid/2050307417163373696; Seismic velocity structure in and around the Naruko volcano, NE Japan, and its implications for volcanic and seismic activities; https://cir.nii.ac.jp/crid/2050307417163386112; 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; Seismic attenuation beneath Kanto, Japan : evidence for high attenuation in the serpentinized subducting mantle; https://cir.nii.ac.jp/crid/2051433317070207104
• 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; 学術機関リポジトリデータベース; https://irdb.nii.ac.jp
• 書誌ID（NDLBibID）: 10319684; http://id.ndl.go.jp/bib/10319684