Anelastic properties beneath the Niigata-Kobe Tectonic Zone, Japan
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DOI[10.1186/s40623-017-0619-1]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Junichi NakajimaToru Matsuzawa
- Publication, Distribution, etc.
- Publication Date
- 2017-02-22
- Publication Date (W3CDTF)
- 2017-02-22
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 69(33)
- Volume
- 69(33)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-017-0619-1
- Persistent ID (NDL)
- info:ndljp/pid/10319684
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2017-04-04T20:19:14+09:00
- Date Captured (W3CDTF)
- 2017-03-24
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/10319651
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- 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
- Access Restrictions
- インターネット公開
- Related Material
- Anelastic properties beneath the Niigata-Kobe Tectonic Zone, Japan
- Related Material (URI)
- Is Referenced By
- Crustal dynamics: unified understanding of geodynamic processes at different time and length scalesSpatiotemporal changes in the strain field in the Niigata–Kobe Tectonic Zone: long-term analysis using GNSS time series dataHigh-resolution three-dimensional azimuthal velocity anisotropy of S-waves in southern-central Japan, based on ambient noise tomographyHigh-Resolution Three-dimensional Azimuthal Velocity Anisotropy of S-waves in southwest Japan, based on Ambient Noise TomographyGenerative Adversarial Networks-Based Ground-Motion Model for Crustal Earthquakes in Japan Considering Detailed Site ConditionsDetection of temporal change in near-source attenuation during intense fluid-driven seismicity following the 2011 Tohoku-Oki earthquake地殻流体の起源・分布と変動現象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 zoneTemporal 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
- References
- Three-dimensional seismic velocity structure and configuration of the Philippine Sea slab in southwestern Japan estimated by double-difference tomographySeismotectonics beneath the Tokyo metropolitan area, Japan: Effect of slab-slab contact and overlap on seismicitySeismic attenuation tomography of the Southwest Japan arc: new insight into subduction dynamicsPlate convergence and long‐term crustal deformation in central JapanImaging P and S attenuation in the termination region of the Hikurangi subduction zone, New ZealandContinuous GPS Array and Present-day Crustal Deformation of JapanLateral variation of the cutoff depth of shallow earthquakes beneath the Japan Islands and its implications for seismogenesisSeismic attenuation beneath northeastern Japan: Constraints on mantle dynamics and arc magmatismNorthern California Seismic Attenuation: 3D<i>Q</i><sub><i>P</i></sub>and<i>Q</i><sub><i>S</i></sub>ModelsGrainsize evolution in ductile shear zones: Implications for strain localization and the strength of the lithosphereSpatial 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 dataGrain‐size‐sensitive seismic wave attenuation in polycrystalline olivineDeep crustal structure along the Niigata-Kobe Tectonic Zone, Japan: Its origin and segmentationSlab‐derived fluids, fore‐arc hydration, and sub‐arc magmatism beneath Kyushu, JapanDouble-planed structure of the deep seismic zone in the northeastern Japan arcSeismic attenuation and mantle wedge temperatures in the Alaska subduction zoneP wave attenuation structure in the fault area of the 1995 Kobe earthquakeWater-weakened lower crust and its role in the concentrated deformation in the Japanese IslandsSeismic velocity structure of the crust beneath the Japan IslandsThe relationship between Late Cenozoic tectonic events and stress field and basin development in northeast JapanSeismic velocities in mantle minerals and the mineralogy of the upper mantleTectonic stress and the spectra of seismic shear waves from earthquakesDeep structure of the northeastern Japan arc and its implications for crustal deformation and shallow seismic activityStrain accumulation process around the Atotsugawa fault system in the Niigata-Kobe Tectonic Zone, central JapanTomographic imaging of <i>P</i> and <i>S</i> wave velocity structure beneath northeastern JapanSource parameters of a M4.8 and its accompanying repeating earthquakes off Kamaishi, NE Japan: Implications for the hierarchical structure of asperities and earthquake cycleImplications of fault-valve behaviour for rupture nucleation and recurrenceAttenuation of seismic waves in dry and saturated rocks; I, Laboratory measurementsGeothermal gradient and heat flow data in and around Japan (I): apprasial of heat flow from geothermal gradient dataMid-crustal electrical conductors and their correlations to seismicity and deformation at Itoigawa-Shizuoka Tectonic LineOrigin of the concentrated deformation zone in the Japanese Islands and stress accumulation process of intraplate earthquakesDislocation model for strain accumulation in a plate collision zoneHeterogeneous crustal deformation along the central-northern Itoigawa-Shizuoka Tectonic Line Fault system, Central Japan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High-resolution map of Coda Q in Japan and their interpretation by the brittle-ductile interaction hypothesisGeochemical evidence for enhanced fluid flux due to overlapping subducting platesSpatial variation in coda Q and stressing rate around the Atotsugawa fault zone in a high strain rate zone, central JapanPore pressure distribution in the focal region of the 2008 M7.2 Iwate-Miyagi Nairiku earthquakeSeismic velocity structure in and around the Naruko volcano, NE Japan, and its implications for volcanic and seismic activitiesSpatial variation in shear wave splitting of the upper crust in the zone of inland high strain rate, central JapanSeismic attenuation beneath Kanto, Japan : evidence for high attenuation in the serpentinized subducting mantle
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース学術機関リポジトリデータベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10319684