Estimate of the contraction rate of central Japan through the deformation of the Philippine Sea slab
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DOI[10.1186/s40645-018-0251-0]のデータに遷移します
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- 資料種別
- 記事
- タイトル
- 著者・編者
- Yukitoshi Fukahata
- 出版年月日等
- 2019-01-15
- 出版年（W3CDTF）
- 2019-01-15
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 6(4)
- 掲載巻
- 6(4)
- 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/s40645-018-0251-0
- 国立国会図書館永続的識別子
- info:ndljp/pid/11249492
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- 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
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2019-03-05T23:10:26+09:00
- 保存日（W3CDTF）
- 2019-03-05
- 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（国立国会図書館永続的識別子）
- info:ndljp/pid/11249488
- 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
- 要約等
- The Philippine Sea (PHS) slab is severely deformed beneath central Japan, but it is subject to little deformation before the subduction along the Nankai Trough. Thus, it is considered that the currently observed deformation of the PHS slab has been formed only after the subduction along the Nankai Trough. This study estimates the contraction rate of the PHS slab along segments roughly parallel to the Nankai Trough, assuming that the configuration of the PHS slab is stationary in time in the coordinate system fixed to the overriding plate. Results show that the contraction rate is small beneath most parts of Shikoku (≤ 0.3 mm/year) and the offshore fore-arc (≤ 0.6 mm/year), while it increases from the Pacific coastal region (3–6 mm/year) to the inland region (approximately 20 mm/year) beneath central Japan. Considering various error sources, the strain rate is estimated to be about 4–7 × 10⁻⁸/year beneath the inland region of central Japan, although it could be reduced by about 20% if the PHS slab has a tear beneath the Kii Strait. Due to the geographical concordance of the deformation between the PHS slab and the upper crust above the slab, the contraction rate of the PHS slab could be used as a proxy to provide an independent estimate of the crustal deformation rate of central Japan over the long term, which is slower than the geodetic estimate while faster than the geologic one.
- DOI
- 10.1186/s40645-018-0251-0
- オンライン閲覧公開範囲
- インターネット公開
- 著作権情報
- © The Author(s). 2019. This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
- 関連情報（URI）
- 参照
- Detection of plastic strain using GNSS data of pre- and post-seismic deformation of the 2011 Tohoku-oki earthquakeStress change in southwest Japan due to the 1944–1946 Nankai megathrust rupture sequence based on a 3-D heterogeneous rheological modelStatistical Characteristics of Strong Earthquake Sequence in Northeastern Tibetan PlateauEffects of Hot Plumes and Slab Rheology on the Bending of the Philippine Sea Slab at Shallow Depths Beneath the Kyushu Region, Southwest Japan
- 参照
- Imaging the fault zones of the 2000 western Tottori earthquake by a new inversion method to estimate three-dimensional distribution of the scattering coefficientThree-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 seismicitySubduction of the Philippine Sea plate beneath southwestern Japan: Slab geometry and its relationship to arc magmatismCoseismic displacement due to the 2008 Iwate-Miyagi Nairiku earthquake detected by ALOS/PALSAR : preliminary resultsPlate convergence and long‐term crustal deformation in central JapanStresses in the subducting slab beneath southwest Japan and relation with plate geometry, tectonic forces, slab dehydration, and damaging earthquakesDeformation of an island arc: Rates of moment release and crustal shortening in intraplate Japan determined from seismicity and Quaternary fault dataContinuous GPS Array and Present-day Crustal Deformation of JapanLandward migration of active folding based on topographic development of folds along the eastern margin of the Japan Sea, northeast JapanSimulation of tectonic evolution of the Kanto Basin of Japan since 1 Ma due to subduction of the Pacific and Philippine Sea plates and the collision of the Izu-Bonin arcA short history of Japanese historical seismology: past and the presentThe 1946 Nankai earthquake and segmentation of the Nankai TroughNew, improved version of generic mapping tools releasedAn updated digital model of plate boundariesTectonic Evolution of the Japanese Island Arc SystemSplit Philippine Sea plate beneath JapanPersistent inelastic deformation in central Japan revealed by GPS observation before and after the Tohoku-oki earthquakeREVEL: A model for Recent plate velocities from space geodesyStriations, duration, migration and tidal response in deep tremorVolcanic history and tectonics of the Southwest Japan ArcA model for the motion of the Philippine Sea Plate consistent with NUVEL‐1 and geological dataGeodynamics of flat subduction: Seismicity and tomographic constraints from the Andean marginPaleogeographic reconstruction and origin of the Philippine SeaSlab1.0: A three‐dimensional model of global subduction zone geometriesIntraplate deformation in the Japanese Islands: A kinematic study of intraplate deformation at a convergent plate marginSlip-line field theory and large-scale continental tectonicsWater-weakened lower crust and its role in the concentrated deformation in the Japanese IslandsThe 3-D tectonic stress fields in and around Japan inverted from centroid moment tensor data of seismic eventsA unified interpretation of vertical movement in Himalaya and horizontal deformation in Tibet on the basis of elastic and viscoelastic dislocation theorySimple relationship between seismic activity along Philippine Sea slab and geometry of oceanic Moho beneath southwest JapanStress, strain, and mountain building in central JapanAn integrated global model of present-day plate motions and plate boundary deformationThe slip distribution of the 1946 Nankai earthquake estimated from tsunami inversion using a new plate model42 A list of deadly earthquakes in the world: 1500–20003-D Modelling of Plate Interfaces and Numerical Simulation of Long-term Crustal Deformation in and around JapanShape of the subducted Rivera and Cocos plates in southern Mexico: Seismic and tectonic implicationsPreceding, coseismic, and postseismic slips of the 2011 Tohoku earthquake, JapanThe Amurian Plate motion and current plate kinematics in eastern AsiaStrain buildup in the Northeast Japan orogen with implications for gigantic subduction earthquakesConfiguration of the Continental Moho and Philippine Sea Slab in Southwest Japan Derived from Receiver Function Analysis: Relation to Subcrustal EarthquakesGeodetic data inversion using a Bayesian information criterion for spatial distribution of fault slipフィリピン海プレートが支配する日本列島のテクトニクス次の南海トラフ巨大地震に備えて フィリピン海スラブの形状Double-Difference Tomography法による関東地方の3次元地震波速度構造およびフィリピン海プレートの形状の推定2008年岩手・宮城内陸地震に伴う地表地震断層?震源過程および活断層評価への示唆?測地測量により求めた日本列島の地震間の平均的な地殻水平歪速度 (I)東北日本島弧−海溝系における長期的歪み蓄積過程と超巨大歪み解放イベントCollision of Izu–Bonin arc with central Honshu. Cenozoic tectonics of the Fossa Magna Japan.Heterogeneous crustal deformation along the central-northern Itoigawa-Shizuoka Tectonic Line Fault system, Central Japan日本列島下のスラブの三次元構造と地震活動東北日本の東西短縮テクトニクスの原因Evolution of the Shikoku Basin.Geochemical evidence for enhanced fluid flux due to overlapping subducting plates
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 学術機関リポジトリデータベース雑誌記事索引データベースCrossrefCiNii Articles科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 11249492
- NII論文ID
- 120006591408