Estimation of slip rate and fault displacement during shallow earthquake rupture in the Nankai subduction zone
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- Material Type
- 記事
- Author/Editor
- Yohei HamadaArito SakaguchiWataru Tanikawa
- Publication, Distribution, etc.
- Publication Date
- 2015-03-13
- Publication Date (W3CDTF)
- 2015-03-13
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 67(39)
- Volume
- 67(39)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-015-0208-0
- Persistent ID (NDL)
- info:ndljp/pid/9381167
- 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)
- 2015-06-08T22:01:55+09:00
- Date Captured (W3CDTF)
- 2015-04-20
- 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/s40623-015-0208-0
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Deformation Structures From Splay and Décollement Faults in the Nankai Accretionary Prism, SW Japan(IODP NanTroSEIZE Expedition 316): Evidence for Slow and Rapid Slip in Fault RocksContinuous depth profile of the rock strength in the Nankai accretionary prism based on drilling performance parametersDeformation Process and Mechanism of the Frontal Megathrust at the Nankai Subduction ZoneExothermic events in a fossil seismogenic fault acquiring thermoviscous remanent magnetization in an exhumed accretionary complexLowering of the kinetic barrier of clay-mineral reactions along a seismogenic fault: Example from the Nankai subduction zone, JapanThree‐dimensional texture of natural pseudotachylyte: Pseudotachylyte formation mechanism in hydrous accretionary complex科学掘削による地震断層の応力状態・物性・すべりパラメーターの評価南海トラフ地震発生帯掘削がもたらした沈み込み帯の新しい描像Kinetic effect of heating rate on the thermal maturity of carbonaceous material as an indicator of frictional heat during earthquakes
- References
- High‐velocity frictional properties of clay‐rich fault gouge in a megasplay fault zone, Nankai subduction zoneEstimation of slip parameters associated with frictional heating during the 1999 Taiwan Chi-Chi earthquake by vitrinite reflectance geothermometryLow Coseismic Shear Stress on the Tohoku-Oki Megathrust Determined from Laboratory ExperimentsCoal maturation by frictional heat during rapid fault slipThree-Dimensional Splay Fault Geometry and Implications for Tsunami GenerationPlate convergence and long‐term crustal deformation in central JapanThermal history estimation of the Taiwan Chelungpu fault using rock‐magnetic methodsFrictional and hydrologic properties of clay‐rich fault gougeContiguous rupture areas of two Nankai Trough earthquakes revealed by high‐resolution tsunami waveform inversionSource mechanisms and tectonic significance of historical earthquakes along the nankai trough, JapanCoseismic frictional heating and fluid-rock interaction in a slip zone within a shallow accretionary prism and implications for earthquake slip behaviorThermal maturity of a fold–thrust belt based on vitrinite reflectance analysis in the Western Foothills complex, western TaiwanShallow Dynamic Overshoot and Energetic Deep Rupture in the 2011 <i>M</i> <sub>w</sub> 9.0 Tohoku-Oki EarthquakeProgressive illitization in fault gouge caused by seismic slip propagation along a megasplay fault in the Nankai TroughRe-evaluation of frictional heat recorded in the dark gouge of the shallow part of a megasplay fault at the Nankai TroughSplay Fault Branching Along the Nankai Subduction ZoneSeismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on Integrated Ocean Drilling Program NanTro SEIZE coresThe Philippine Sea: New survey results reveal the structure and the history of the marginal basinsNanTroSEIZE: The IODP Nankai Trough Seismogenic Zone ExperimentNanTroSEIZE Stage 1: NanTroSEIZE Shallow Megasplay and Frontal Thrusts AddendumVitrinite reflectance and shear-induced graphitization in orogenic belts: A case study from the Kandersteg area, Helvetic Alps, SwitzerlandChanges to magnetic minerals caused by frictional heating during the 1999 Taiwan Chi-Chi earthquakeExperimental frictional heating of coal gouge at seismic slip rates: Evidence for devolatilization and thermal pressurization of gouge fluidsEstimated dynamic shear stress and frictional heat during the 1999 Taiwan Chi-Chi earthquake: A chemical kinetics approach with isothermal heating experimentsRupture process of the 1944 Tonankai earthquake (<i>M</i><sub><i>s</i></sub> 8.1) from the inversion of teleseismic and regional seismogramsCoseismic fluid–rock interactions at high temperatures in the Chelungpu faultA chemical kinetic approach to estimate dynamic shear stress during the 1999 Taiwan Chi‐Chi earthquakeEstimation of temperature rise in a shallow slip zone of the megasplay fault in the Nankai TroughFluid-inclusion technique for determining maximum temperature in calcite and its comparison to the vitrinite reflectance geothermometerHigh precision slip distribution of the 1944 Tonankai earthquake inferred from tsunami waveforms: Possible slip on a splay faultHeating during thrust faulting in the rocky mountains: friction or fiction?Earthquakes and friction lawsThermal considerations in inferring frictional heating from vitrinite reflectance and implications for shallow coseismic slip within the Nankai Subduction ZoneVery low frequency earthquakes excited by the 2004 off Kii peninsula earthquakes: a dynamic deformation process in the large accretionary prismSource rupture process of the 1944 Tonankai earthquake and the 1945 Mikawa earthquake derived from low-gain seismogramsCoseismic slip distribution of the 1946 Nankai earthquake and aseismic slips caused by the earthquakeLow‐frequency tremors associated with reverse faults in a shallow accretionary prismGeochemical and mineralogical characteristics of fault gouge in the Median Tectonic Line, Japan : evidence for earthquake slip
- 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CrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 9381167