Stress state in the upper crust around the source region of the 1891 Nobi earthquake through shear wave polarization anisotropy
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DOI[10.1186/s40623-015-0220-4]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Yoshihiro HiramatsuTakashi IidakaThe research group for the joint seismic observations at the Nobi area
- Publication, Distribution, etc.
- Publication Date
- 2015-04-17
- Publication Date (W3CDTF)
- 2015-04-17
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 67(52)
- Volume
- 67(52)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-015-0220-4
- Persistent ID (NDL)
- info:ndljp/pid/9483537
- 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)
- 2015-08-17T20:47:01+09:00
- Date Captured (W3CDTF)
- 2015-06-20
- 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/9227920
- 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/s40623-015-0220-4
- Related Material (URI)
- Is Referenced By
- Focal mechanisms and stress field in the Nobi fault area, central JapanHigh-Resolution Three-dimensional Azimuthal Velocity Anisotropy of S-waves in southwest Japan, based on Ambient Noise TomographySpatial variation in coda Q in the northeastern part of Niigata–Kobe Tectonic Zone, central Japan : implication of the cause of a high strain rate zoneHeterogeneous mantle anisotropy and fluid upwelling : implication for generation of the 1891 Nobi earthquake
- References
- Changes in Seismic Anisotropy After Volcanic Eruptions: Evidence from Mount RuapehuShear-wave polarizations on a curved wavefront at an isotropic free surfaceOrigin of crustal anisotropy: Shear Wave splitting studies in JapanNew, improved version of generic mapping tools releasedSpontaneous Rupture Propagation on a Non-planar Fault in 3-D Elastic MediumStress magnitude and its temporal variation at Mt. Asama Volcano, Japan, from seismic anisotropy and GPSEvidence for rapid fault healing derived from temporal changes in <i>S</i> wave splittingDeep crustal structure along the Niigata-Kobe Tectonic Zone, Japan: Its origin and segmentationShear-wave anisotropy: spatial and temporal variations in time delays at Parkfield, Central CaliforniaSeismological evidence on characteristic time of crack healing in the shallow crustWater-weakened lower crust and its role in the concentrated deformation in the Japanese IslandsSpatial variation in the crustal anisotropy and its temporal variation associated with a moderate-sized earthquake in the Tokai region, central JapanThe 3-D tectonic stress fields in and around Japan inverted from centroid moment tensor data of seismic eventsStress‐induced spatiotemporal variations in anisotropic structures beneath Hakone volcano, Japan, detected by <i>S</i> wave splitting: A tool for volcanic activity monitoringStress, strain, and mountain building in central JapanThree-dimensional P- and S-wave velocity structures beneath the Japan Islands obtained by high-density seismic stations by seismic tomographyShear wave splitting and subcontinental mantle deformationAnalysis and forward modeling of seismic anisotropy during the ongoing eruption of the Soufrière Hills Volcano, Montserrat, 1996–2007Coseismic Change and Recovery of Scattering Environment in the Crust after the 1995 Hyogo-ken Nanbu Earthquake, Japan本州中央部の地殻応力方位分布―応力区とその成因High-resolution map of Coda Q in Japan and their interpretation by the brittle-ductile interaction hypothesisSpatial variation in coda Q and stressing rate around the Atotsugawa fault zone in a high strain rate zone, central JapanSpatial variation in coda Q around the Nobi fault zone, central Japan : relation to S-wave velocity and seismicitySpatial variation in shear wave splitting of the upper crust in the zone of inland high strain rate, central Japan
- 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CrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 9483537