Punctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough
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- Material Type
- 記事
- Author/Editor
- Gaku KimuraHiroaki KogeTakeshi Tsuji
- Publication, Distribution, etc.
- Publication Date
- 2018-11-21
- Publication Date (W3CDTF)
- 2018-11-21
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 5(78)
- Volume
- 5(78)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-018-0234-1
- Persistent ID (NDL)
- info:ndljp/pid/11190373
- 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)
- 2018-11-26T20:20:20+09:00
- Date Captured (W3CDTF)
- 2018-11-26
- 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/11018906
- 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/s40645-018-0234-1
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Multiple Types of Porosity – P‐Wave Velocity Relationships for the Nankai TroughRejuvenated extension of the Philippine Sea plate and its effect on subduction dynamics in the Nankai TroughHeterogeneous Sediment Input at the Nankai Trough Subduction Zone: Implications for Shallow Slow Earthquake LocalizationDécollement geometry controls on shallow very low frequency earthquakesNankai Forearc Structural and Seismogenic Segmentation Caused by a Magmatic Intrusion off the Kii PeninsulaThermogenic methane and hydrogen generation in subducted sediments of the Nankai TroughShallow structure and late quaternary slip rate of the Osaka Bay fault, western Japanジュラ系智頭コンプレックス中にみられるテクトニック・メランジュの変形構造Quantitative logging data clustering with hidden Markov model to assist log unit classificationPaleo-stress orientations and magnitudes from triaxial testing and stress inversion analysis in Nankai accretionary prism sedimentsA new method for the empirical conversion of logging data to clay mineral fraction in the Nankai accretionary prism
- References
- Connecting slow earthquakes to large earthquakesMiddle Miocene swift migration of the TTT triple junction and rapid crustal growth in southwest Japan: A reviewIdentification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai Trough3D geometry of a plate boundary fault related to the 2016 Off-Mie earthquake in the Nankai subduction zone, JapanBack‐arc opening and the mode of subductionA cause of rupture segmentation and synchronization in the Nankai trough revealed by seismic imaging and numerical simulationReinitiation of subduction and magmatic responses in SW Japan during Neogene timeRapid forearc basin uplift and megasplay fault development from 3D seismic images of Nankai Margin off Kii Peninsula, JapanGeologically current motion of 56 plates relative to the no-net-rotation reference frameThe origin of strata within the inner accretionary prism of Nankai Trough: Evidence from clay mineral assemblages along the NanTroSEIZE transectStructural and seismic stratigraphic framework of the NanTroSEIZE Stage 1 transectLarge Mass Transport Deposits in Kumano Basin, Nankai Trough, JapanTriple junctions as a cause for anomalously near-trench igneous activity between the trench and volcanic arcDepositional architecture, provenance, and tectonic/eustatic modulation of Miocene submarine fans in the Shikoku Basin: Results from <b>Nankai Trough Seismogenic Zone Experiment</b>Subducted Seamount Imaged in the Rupture Zone of the 1946 Nankaido EarthquakeCrustal velocity field of southwest Japan: Subduction and arc‐arc collisionInteractions between deformation and fluids in the frontal thrust region of the NanTroSEIZE transect offshore the Kii Peninsula, Japan: Results from IODP Expedition 316 Sites C0006 and C0007Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animationsExpedition 315 summaryA low-velocity zone with weak reflectivity along the Nankai subduction zoneDeformation of the Nankai Trough inner accretionary prism: The role of inherited structuresEvolution of tectono-sedimentary systems in the Kumano Basin, Nankai Trough forearcEvolution of Sedimentary Environments in the Subduction Zone v of Southwest Japan: Recent Results from the NanTroSEIZE Kumano TransectGeologically current plate motionsPhilippine Sea and East Asian plate tectonics since 52 Ma constrained by new subducted slab reconstruction methodsPossible strain partitioning structure between the Kumano fore‐arc basin and the slope of the Nankai Trough accretionary prismSpatial and temporal evolution of the megasplay fault in the Nankai TroughCharacterization of hydrate and gas reservoirs in plate convergent margin by applying rock physics to high-resolution seismic velocity modelRecurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrustSpreading process of the northern Mariana Trough: Rifting‐spreading transition at 22°NVolcanic history and tectonics of the Southwest Japan ArcNanTroSEIZE: The IODP Nankai Trough Seismogenic Zone ExperimentZircon and apatite thermochronology of the Nankai Trough accretionary prism and trench, Japan: Sediment transport in an active and collisional margin settingDynamics of the Ryukyu/Izu-Bonin-Marianas double subduction systemMechanism of backarc opening in the Japan Sea: role of asthenospheric injectionExpedition 319 summaryPropagating extrusion tectonics in Asia: New insights from simple experiments with plasticineMantle Flow and Deforming Continents: From India‐Asia Convergence to Pacific SubductionPlate motions, slab dynamics and back-arc deformationExpedition 316 Site C0006Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stressRidge subduction sparked reorganization of the Pacific plate‐mantle system 60–50 million years agoDetermination of the Amurian plate motionOn acoustic waveform tomography of wide-angle OBS data--strategies for pre-conditioning and inversionOrigin and development of marginal basins in the western PacificEpisodic exhumation of accretionary complexes: Fission‐track thermochronologic evidence from the Shimanto Belt and its vicinities, southwest JapanTransition of accretionary wedge structures around the up-dip limit of the seismogenic subduction zoneInitial Reports of the Deep Sea Drilling Project, 60Progressive Melt Extraction from Upwelling Mantle Constrained by the Kita-Matsuura Basalts in NW Kyushu, SW JapanIncipient subduction and deduction along the eastern margin of the Japan SeaFault‐related folds above the source fault of the 2004 mid‐Niigata Prefecture earthquake, in a fold‐and‐thrust belt caused by basin inversion along the eastern margin of the Japan SeaPore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zone紀伊半島東南部の熊野層群の地質と堆積西南日本弧前縁の圧縮テクトニクスと中期中新世カルデラ火山Origin and evolution of a splay fault in the Nankai accretionary wedgeStrike-slip motion of a mega-splay fault system in the Nankai oblique subduction zone
- 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CrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11190373