Punctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough

• 資料種別: 記事
• タイトル: Punctuated growth of an accretionary prism and the onset of a seismogenic megathrust in the Nankai Trough
• 著者・編者: Gaku Kimura; Hiroaki Koge; Takeshi Tsuji
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2018-11-21
• 出版年（W3CDTF）: 2018-11-21
• タイトル（掲載誌）: Progress in earth and planetary science
• 巻号年月日等（掲載誌）: 5(78)
• 掲載巻: 5(78)
• ISSN（掲載誌）: 2197-4284
• ISSN-L（掲載誌）: 2197-4284
• 本文の言語コード: eng
• DOI: 10.1186/s40645-018-0234-1; https://doi.org/10.1186/s40645-018-0234-1
• 国立国会図書館永続的識別子: info:ndljp/pid/11190373; https://dl.ndl.go.jp/pid/11190373
• 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）: 2018-11-26T20:20:20+09:00
• 保存日（W3CDTF）: 2018-11-26
• 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）: https://progearthplanetsci.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/11018906; https://dl.ndl.go.jp/pid/11018906
• 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/s40645-018-0234-1; https://doi.org/10.1186/s40645-018-0234-1
• オンライン閲覧公開範囲: インターネット公開
• 関連情報（URI）: http://id.ndl.go.jp/digimeta/11190373; https://dl.ndl.go.jp/pid/11190373; http://link.springer.com/content/pdf/10.1186/s40645-018-0234-1.pdf; http://link.springer.com/article/10.1186/s40645-018-0234-1/fulltext.html
• 参照: Multiple Types of Porosity – P‐Wave Velocity Relationships for the Nankai Trough; https://cir.nii.ac.jp/crid/1360298757432546176; Rejuvenated extension of the Philippine Sea plate and its effect on subduction dynamics in the Nankai Trough; https://cir.nii.ac.jp/crid/1360572092541173504; Heterogeneous Sediment Input at the Nankai Trough Subduction Zone: Implications for Shallow Slow Earthquake Localization; https://cir.nii.ac.jp/crid/1360854882786727936; Décollement geometry controls on shallow very low frequency earthquakes; https://cir.nii.ac.jp/crid/1360857593797072640; Nankai Forearc Structural and Seismogenic Segmentation Caused by a Magmatic Intrusion off the Kii Peninsula; https://cir.nii.ac.jp/crid/1360861294960273280; Thermogenic methane and hydrogen generation in subducted sediments of the Nankai Trough; https://cir.nii.ac.jp/crid/1360865815686076672; Shallow structure and late quaternary slip rate of the Osaka Bay fault, western Japan; https://cir.nii.ac.jp/crid/1360869854375589632; 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; https://cir.nii.ac.jp/crid/1390287474423766656; Quantitative logging data clustering with hidden Markov model to assist log unit classification; https://cir.nii.ac.jp/crid/2050588892108506240; Paleo-stress orientations and magnitudes from triaxial testing and stress inversion analysis in Nankai accretionary prism sediments; https://cir.nii.ac.jp/crid/2051151842043307392; A new method for the empirical conversion of logging data to clay mineral fraction in the Nankai accretionary prism; https://cir.nii.ac.jp/crid/2051151842051758976
• 参照: Connecting slow earthquakes to large earthquakes; https://cir.nii.ac.jp/crid/1050001339107234432; Middle Miocene swift migration of the TTT triple junction and rapid crustal growth in southwest Japan: A review; https://cir.nii.ac.jp/crid/1360002214349470592; Identification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai Trough; https://cir.nii.ac.jp/crid/1360002215916314624; 3D geometry of a plate boundary fault related to the 2016 Off-Mie earthquake in the Nankai subduction zone, Japan; https://cir.nii.ac.jp/crid/1360004232135547264; Back‐arc opening and the mode of subduction; https://cir.nii.ac.jp/crid/1360011142930078848; A cause of rupture segmentation and synchronization in the Nankai trough revealed by seismic imaging and numerical simulation; https://cir.nii.ac.jp/crid/1360011142931982336; Reinitiation of subduction and magmatic responses in SW Japan during Neogene time; https://cir.nii.ac.jp/crid/1360011142933108480; Rapid forearc basin uplift and megasplay fault development from 3D seismic images of Nankai Margin off Kii Peninsula, Japan; https://cir.nii.ac.jp/crid/1360011142937696896; Geologically current motion of 56 plates relative to the no-net-rotation reference frame; https://cir.nii.ac.jp/crid/1360011142940256896; The origin of strata within the inner accretionary prism of Nankai Trough: Evidence from clay mineral assemblages along the NanTroSEIZE transect; https://cir.nii.ac.jp/crid/1360011142941276544; Structural and seismic stratigraphic framework of the NanTroSEIZE Stage 1 transect; https://cir.nii.ac.jp/crid/1360011145011126528; Large Mass Transport Deposits in Kumano Basin, Nankai Trough, Japan; https://cir.nii.ac.jp/crid/1360011145509602304; Triple junctions as a cause for anomalously near-trench igneous activity between the trench and volcanic arc; https://cir.nii.ac.jp/crid/1360011146583418112; Depositional architecture, provenance, and tectonic/eustatic modulation of Miocene submarine fans in the Shikoku Basin: Results from <b>Nankai Trough Seismogenic Zone Experiment</b>; https://cir.nii.ac.jp/crid/1360285705096204928; Subducted Seamount Imaged in the Rupture Zone of the 1946 Nankaido Earthquake; https://cir.nii.ac.jp/crid/1360292617907095680; Crustal velocity field of southwest Japan: Subduction and arc‐arc collision; https://cir.nii.ac.jp/crid/1360292617909503360; Interactions 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 C0007; https://cir.nii.ac.jp/crid/1360292617911270528; Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations; https://cir.nii.ac.jp/crid/1360292617916137216; Expedition 315 summary; https://cir.nii.ac.jp/crid/1360292619349685760; A low-velocity zone with weak reflectivity along the Nankai subduction zone; https://cir.nii.ac.jp/crid/1360565168428104704; Deformation of the Nankai Trough inner accretionary prism: The role of inherited structures; https://cir.nii.ac.jp/crid/1360574092884179712; Evolution of tectono-sedimentary systems in the Kumano Basin, Nankai Trough forearc; https://cir.nii.ac.jp/crid/1360574092886141056; Evolution of Sedimentary Environments in the Subduction Zone v of Southwest Japan: Recent Results from the NanTroSEIZE Kumano Transect; https://cir.nii.ac.jp/crid/1360574092886847488; Geologically current plate motions; https://cir.nii.ac.jp/crid/1360574092887403392; Philippine Sea and East Asian plate tectonics since 52 Ma constrained by new subducted slab reconstruction methods; https://cir.nii.ac.jp/crid/1360574092887737984; Possible strain partitioning structure between the Kumano fore‐arc basin and the slope of the Nankai Trough accretionary prism; https://cir.nii.ac.jp/crid/1360574092892046336; Spatial and temporal evolution of the megasplay fault in the Nankai Trough; https://cir.nii.ac.jp/crid/1360574096581186304; Characterization of hydrate and gas reservoirs in plate convergent margin by applying rock physics to high-resolution seismic velocity model; https://cir.nii.ac.jp/crid/1360846640994414720; Recurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrust; https://cir.nii.ac.jp/crid/1360846643379862144; Spreading process of the northern Mariana Trough: Rifting‐spreading transition at 22°N; https://cir.nii.ac.jp/crid/1360855567862929664; Volcanic history and tectonics of the Southwest Japan Arc; https://cir.nii.ac.jp/crid/1360855567863071232; NanTroSEIZE: The IODP Nankai Trough Seismogenic Zone Experiment; https://cir.nii.ac.jp/crid/1360855567869180160; Zircon and apatite thermochronology of the Nankai Trough accretionary prism and trench, Japan: Sediment transport in an active and collisional margin setting; https://cir.nii.ac.jp/crid/1360855567870200448; Dynamics of the Ryukyu/Izu-Bonin-Marianas double subduction system; https://cir.nii.ac.jp/crid/1360855567870334976; Mechanism of backarc opening in the Japan Sea: role of asthenospheric injection; https://cir.nii.ac.jp/crid/1360855568521631360; Expedition 319 summary; https://cir.nii.ac.jp/crid/1360855571245354752; Propagating extrusion tectonics in Asia: New insights from simple experiments with plasticine; https://cir.nii.ac.jp/crid/1361699995646141184; Mantle Flow and Deforming Continents: From India‐Asia Convergence to Pacific Subduction; https://cir.nii.ac.jp/crid/1361699995673397888; Plate motions, slab dynamics and back-arc deformation; https://cir.nii.ac.jp/crid/1361699996033209088; Expedition 316 Site C0006; https://cir.nii.ac.jp/crid/1361981468452281344; Updip limit of the seismogenic zone beneath the accretionary prism of southwest Japan: An effect of diagenetic to low-grade metamorphic processes and increasing effective stress; https://cir.nii.ac.jp/crid/1361981471029956480; Ridge subduction sparked reorganization of the Pacific plate‐mantle system 60–50 million years ago; https://cir.nii.ac.jp/crid/1361981471284832256; Determination of the Amurian plate motion; https://cir.nii.ac.jp/crid/1361981471465123072; On acoustic waveform tomography of wide-angle OBS data--strategies for pre-conditioning and inversion; https://cir.nii.ac.jp/crid/1362262944462664576; Origin and development of marginal basins in the western Pacific; https://cir.nii.ac.jp/crid/1362544418875456640; Episodic exhumation of accretionary complexes: Fission‐track thermochronologic evidence from the Shimanto Belt and its vicinities, southwest Japan; https://cir.nii.ac.jp/crid/1362544420194023808; Transition of accretionary wedge structures around the up-dip limit of the seismogenic subduction zone; https://cir.nii.ac.jp/crid/1362544420753100544; Initial Reports of the Deep Sea Drilling Project, 60; https://cir.nii.ac.jp/crid/1362825894757073280; Progressive Melt Extraction from Upwelling Mantle Constrained by the Kita-Matsuura Basalts in NW Kyushu, SW Japan; https://cir.nii.ac.jp/crid/1363388846172333568; Incipient subduction and deduction along the eastern margin of the Japan Sea; https://cir.nii.ac.jp/crid/1363670318283380224; Fault‐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 Sea; https://cir.nii.ac.jp/crid/1363951795515673600; Pore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zone; https://cir.nii.ac.jp/crid/1364233270495213440; 紀伊半島東南部の熊野層群の地質と堆積; https://cir.nii.ac.jp/crid/1390001206238387584; 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; https://cir.nii.ac.jp/crid/1390282681213579136; Origin and evolution of a splay fault in the Nankai accretionary wedge; https://cir.nii.ac.jp/crid/1571417126454293760; Strike-slip motion of a mega-splay fault system in the Nankai oblique subduction zone; https://cir.nii.ac.jp/crid/2051996267023651328
• 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
• 書誌ID（NDLBibID）: 11190373; http://id.ndl.go.jp/bib/11190373