Upper boundaries of the Pacific and Philippine Sea plates near the triple junction off the Boso Peninsula deduced from ocean-bottom seismic observations
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DOI[10.1186/s40623-017-0608-4]のデータに遷移します
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- 資料種別
- 記事
- 著者・編者
- Aki ItoHiroko SugiokaKoichiro Obana
- 出版年月日等
- 2017-02-09
- 出版年（W3CDTF）
- 2017-02-09
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 69(30)
- 掲載巻
- 69(30)
- ISSN（掲載誌）
- 1880-5981
- ISSN-L（掲載誌）
- 1343-8832
- 本文の言語コード
- eng
- DOI
- 10.1186/s40623-017-0608-4
- 国立国会図書館永続的識別子
- info:ndljp/pid/10319681
- 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）
- 2017-04-04T20:19:14+09:00
- 保存日（W3CDTF）
- 2017-03-24
- 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/10319651
- 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
- We determined hypocenter distributions and focal mechanisms of earthquakes off the Boso Peninsula, Japan, based on seafloor observations using ocean-bottom seismometers (OBSs). From OBS data, we detected and located earthquakes that were closer to the trenches than had previously been reported. The determined focal depths of relocated hypocenters were systematically shallower than those in the Japan Meteorological Agency catalog determined from land-based data. The hypocenter distribution was separated into two groups: one associated with the Pacific plate (PAC) and the other with the North American and/or Philippine Sea plates (PHS). For the former group, both the focal depths and mechanisms of low-angle thrust-faulting earthquakes were consistent with the geometry of the PAC determined by previous studies. Among the latter group, we selected low-angle thrust-faulting earthquakes with a slip direction parallel to the direction of PHS subduction or with a dip direction parallel to the PHS to delineate the upper boundary of the PHS. The depth of the plate upper boundary off the Boso Peninsula was found to be approximately 6 km shallower than previously reported estimates.
- DOI
- 10.1186/s40623-017-0608-4
- 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) 2017.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
- MOESM3 of Upper boundaries of the Pacific and Philippine Sea plates near the triple junction off the Boso Peninsula deduced from ocean-bottom seismic observationsMOESM2 of Upper boundaries of the Pacific and Philippine Sea plates near the triple junction off the Boso Peninsula deduced from ocean-bottom seismic observationsMOESM1 of Upper boundaries of the Pacific and Philippine Sea plates near the triple junction off the Boso Peninsula deduced from ocean-bottom seismic observationsMOESM4 of Upper boundaries of the Pacific and Philippine Sea plates near the triple junction off the Boso Peninsula deduced from ocean-bottom seismic observations
- 関連情報（URI）
- 参照
- Migration-Based Local Event-Location Workflow for Ocean-Bottom Seismometer (OBS) Records in Subduction Zones: A Practical Approach for Addressing a Large Number of EventsSlow Slip Events in the Kanto and Tokai Regions of Central Japan Detected Using Global Navigation Satellite System Data During 1994–2020Long-period ground motion simulation using centroid moment tensor inversion solutions based on the regional three-dimensional model in the Kanto region, JapanConfiguration and structure of the Philippine Sea Plate off Boso, Japan: constraints on the shallow subduction kinematics, seismicity, and slow slip eventsTomographic image of crust and upper mantle off the Boso Peninsula using data from an ocean-bottom seismograph array
- 参照
- Acceleration of regional plate subduction beneath Kanto, Japan, after the 2011 Tohoku‐oki earthquakeThe source model and recurrence interval of Genroku-type Kanto earthquakes estimated from paleo-shoreline dataThe Boso slow slip events in 2007 and 2011 as a driving process for the accompanying earthquake swarmAftershocks near the updip end of the 2011 Tohoku-Oki earthquakeTime and Space Distribution of Coseismic Slip of the 2011 Tohoku Earthquake as Inferred from Tsunami Waveform DataChange in stress field after the 2011 great Tohoku-Oki earthquakeThe global CMT project 2004–2010: Centroid-moment tensors for 13,017 earthquakesPrecise aftershock distribution of the 2011 off the Pacific coast of Tohoku Earthquake revealed by an ocean-bottom seismometer networkRupture process of the 2011 Tohoku-oki earthquake and absolute elastic strain releaseWidespread seismicity excitation throughout central Japan following the 2011 M=9.0 Tohoku earthquake and its interpretation by Coulomb stress transferSpatial distribution and focal mechanisms of aftershocks of the 2011 off the Pacific coast of Tohoku EarthquakeAftershock observation of the 2011 off the Pacific coast of Tohoku Earthquake by using ocean bottom seismometer networkSupraslab earthquake clusters above the subduction plate boundary offshore Sanriku, northeastern Japan: Seismogenesis in a graveyard of detached seamounts?Geologically current plate motionsInsight into complex rupturing of the immature bending normal fault in the outer slope of the Japan Trench from aftershocks of the 2005 Sanriku earthquake (<i>M</i><sub><i>w</i></sub> = 7.0) located by ocean bottom seismometryWhat controls interplate coupling?: Evidence for abrupt change in coupling across a border between two overlying plates in the NE Japan subduction zone深海用微差圧計の校正手法海底地震観測の最近の進展Seismotectonics beneath the Tokyo metropolitan area, Japan: Effect of slab-slab contact and overlap on seismicityWeak Interplate Coupling by Seamounts and Repeating <i>M</i> ~ 7 EarthquakesGeodetic data inversion based on Bayesian formulation with direct and indirect prior informationSeismic activity associated with the subducting motion of the Philippine Sea plate beneath the Kanto district, JapanAnomalous low velocity zone and linear alignment of seismicity along it in the Pacific slab beneath Kanto, Japan: reactivation of subducted fracture zone?Bending of the subducting oceanic plate and its implication for rupture propagation of large interplate earthquakes off Miyagi, Japan, in the Japan Trench subduction zoneInterplate Coupling in the Kanto District, Central Japan, and the Boso Peninsula Silent Earthquake in May 1996Recent progress of seismic observation networks in JapanHi-net and F-net and K-NET and KiK-netRepeating earthquakes and interplate aseismic slip in the northeastern Japan subduction zoneCharacteristic silent earthquakes in the eastern part of the Boso peninsula, Central Japan85.12 FOCMEC: FOCal MEChanism determinationsAlong‐arc structural variation of the plate boundary at the Japan Trench margin: Implication of interplate couplingProbabilistic Earthquake Location in 3D and Layered ModelsTriangle diagrams: ternary graphs to display similarity and diversity of earthquake focal mechanismsGeometry and relative motion of the Philippine Sea Plate and Pacific Plate beneath the Kanto‐Tokai District, JapanMaximum-likelihood estimation of hypocenter with origin time eliminated using nonlinear inversion techniqueDetermination of earthquake source parameters from waveform data for studies of global and regional seismicity
- 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国立国会図書館デジタルコレクションCrossrefCiNii Articles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CrossrefCrossrefCrossrefCrossrefCrossref
- NII論文ID
- 120006360180