Spatial heterogeneities in tectonic stress in Kyushu, Japan and their relation to a major shear zone
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DOI[10.1186/s40623-015-0342-8]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
- Satoshi MatsumotoShigeru NakaoTakahiro Ohkura
- 出版年月日等
- 2015-10-23
- 出版年（W3CDTF）
- 2015-10-23
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 67(172)
- 掲載巻
- 67(172)
- 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/s40623-015-0342-8
- 国立国会図書館永続的識別子
- info:ndljp/pid/9772866
- 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）
- 2016-02-03T17:25:14+09:00
- 保存日（W3CDTF）
- 2015-12-20
- 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/9227920
- 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 investigated the spatial variation in the stress fields of Kyushu Island, southwestern Japan. Kyushu Island is characterized by active volcanoes (Aso, Unzen, Kirishima, and Sakurajima) and a shear zone (western extension of the median tectonic line). Shallow earthquakes frequently occur not only along active faults but also in the central region of the island, which is characterized by active volcanoes. We evaluated the focal mechanisms of the shallow earthquakes on Kyushu Island to determine the relative deviatoric stress field. Generally, the stress field was estimated by using the method proposed by Hardebeck and Michael (2006) for the strike-slip regime in this area. The minimum principal compression stress (σ3), with its near north-south trend, is dominant throughout the entire region. However, the σ 3 axes around the shear zone are rotated normal to the zone. This result is indicative of shear stress reduction at the zone and is consistent with the right-lateral fault behavior along the zone detected by a strain-rate field analysis with global positioning system data. Conversely, the stress field of the normal fault is dominant in the Beppu-Shimabara area, which is located in the central part of the island. This result and the direction of σ3 are consistent with the formation of a graben structure in the area.
- DOI
- 10.1186/s40623-015-0342-8
- 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
- © 2015 Matsumoto et al. 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
- Volcanic magma reservoir imaged as a low-density body beneath Aso volcano that terminated thr 2016 Kumamoto earthquake ruptureSimultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR dataPrestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (<i>M</i>7.3)Rupture process of the 2016 Kumamoto earthquake in relation with the thermal structure around Aso volcanoAzimuthal differences and changes in strain rate and stress of the Japanese Islands deduced from geophysical dataInelastic strain rate in the seismogenic layer of Kyushu Island, JapanSeismicity controlled by resistivity structure : the 2016 Kumamoto earthquakes, Kyushu Island, JapanCrustal magma pathway beneath Aso caldera inferred from 3-D electrical resistivity structureMagmatic–hydrothermal system of Aso Volcano, Japan, inferred from electrical resistivity structuresEarthquake-induced structural deformations enhance long-term solute fluxes from active volcanic systemsSpatiotemporal Change in the Stress State Around the Hypocentral Area of the 2016 Kumamoto Earthquake SequenceSpatial and temporal seismic velocity changes on Kyushu Island during the 2016 Kumamoto earthquakeRETRACTED ARTICLE: Structural features and seismotectonic implications of coseismic surface ruptures produced by the 2016 Mw 7.1 Kumamoto earthquakeThree‐Dimensional Electrical Resistivity Distribution Beneath the Beppu–Shimabara Graben With a Focus on Aso Caldera, Southwest Japan Subduction ZoneA method for mapping intrinsic attenuation factors and scattering coefficients of<i>S</i>waves in 3-D space and its application in southwestern JapanStrain partitioning and interplate coupling along the northern margin of the Philippine Sea plate, estimated from Global Navigation Satellite System and Global Positioning System-Acoustic dataMagmatic fluid pathways in the upper crust: insights from dense magnetotelluric observations around the Kuju Volcanoes, JapanConstraint on the background stress in the source region of the 2016 Kumamoto earthquake sequence based on temporal changes in elastic strain energies and coseismic stress rotationForeshock migration preceding the 2016 <i>M<sub>w</sub></i> 7.0 Kumamoto earthquake, JapanCoseismic conjugate faulting structures produced by the 2016 M w 7.1 Kumamoto earthquake, JapanPaleostress and fluid-pressure regimes inferred from the orientations of Hishikari low sulfidation epithermal gold veins in southern JapanThree‐Dimensional Electrical Resistivity Modeling to Elucidate the Crustal Magma Supply System Beneath Aso Caldera, JapanHigh-resolution image on terminus of fault rupture: relationship with volcanic hydrothermal structureMethod for estimating the stress field from seismic moment tensor data based on the flow rule in plasticity theoryOn Applications of Fast Domain Partitioning Method to Earthquake Simulations with Spatiotemporal Boundary Integral Equation MethodStress, strain rate and anisotropy in Kyushu, JapanMillennium Recurrence Interval of Morphogenic Earthquakes on the Seismogenic Fault Zone That Triggered the 2016 Mw 7.1 Kumamoto Earthquake, Southwest JapanRevisiting Intraslab Earthquakes Beneath Kyushu, Japan: Effect of Ridge Subduction on Seismogenesis2016年熊本地震で益城町の低地に生じた並走断層群を横断する反射法地震探査The 2016 Kumamoto earthquake sequenceThe Advancement of Research on Inland Earthquake Generation 2014–20182016年熊本地震合同地震観測データ非弾性ひずみ回復法を用いた熊本地震震源域における深度700mまでの地震後応力状態の測定九州中部の第四紀テクトニクスと2016年熊本地震フィッション・トラック熱年代解析およびU-Pb年代測定に基づいた南九州せん断帯に分布する破砕帯の活動時期九州中部の第四紀テクトニクスからみた熊本地震地殻深部から上昇する流体が地震の発生に及ぼす影響の研究Stress and pore fluid pressure control of seismicity rate changes following the 2016 Kumamoto earthquake, JapanThe 2016 Kumamoto-Oita earthquake sequence : aftershock seismicity gap and dynamic triggering in volcanic areasCrustal deformation model of the Beppu-Shimabara graben area, central Kyushu, Japan, based on inversion of three-component GNSS data in 2000-2010Three-dimensional P- and S-wave attenuation structures around the source region of the 2016 Kumamoto earthquakesElectrical conductive fluid-rich zones and their influence on the earthquake initiation, growth, and arrest processes : observations from the 2016 Kumamoto earthquake sequence, Kyushu Island, Japan
- 参照
- Damped regional‐scale stress inversions: Methodology and examples for southern California and the Coalinga aftershock sequenceNew Evidence on the State of Stress of the San Andreas Fault SystemDetermining changes in the state of stress associated with an earthquake via combined focal mechanism and moment tensor analysis: Application to the 2013 Awaji Island earthquake, JapanA New Method for Determining First-Motion Focal MechanismsSyntheses of the regional stress fields of the Japanese islandsModeling heterogeneous deviatoric stress field around the hypocentral area of the 2005 Fukuoka earthquake (M7.0) by spatially distributed moment tensorsVolcanic history and tectonics of the Southwest Japan ArcDetermination of stress from slip data: Faults and foldsDetermination of the mean principal directions of stresses for a given fault populationRegional tectonic stress near the San Andreas fault in central and southern CaliforniaA model with rigid rotations and slip deficits for the GPS-derived velocity field in Southwest JapanThe 3-D tectonic stress fields in and around Japan inverted from centroid moment tensor data of seismic eventsTectonic analysis of fault slip data setsStress, strain, and mountain building in central JapanSlab rollback suggested by latest Miocene to Pliocene forearc stress and migration of volcanic front in southern Kyushu, northern Ryukyu ArcImplications of earthquake focal mechanisms for the frictional strength of the San Andreas fault systemTectonics of an arc-arc junction: an example from Kyushu Island at the junction of the Southwest Japan Arc and the Ryukyu ArcCrustal stress field in southern California and its implications for fault mechanicsEnigmatic, highly active left-lateral shear zone in southwest Japan explained by aseismic ridge collisionAftershock seismicity and fault structure of the 2005 West Off Fukuoka Prefecture Earthquake (MJMA7.0) derived from urgent joint observationsThree-dimensional seismic velocity structure as determined by double-difference tomography in and around the focal area of the 2005 West off Fukuoka Prefecture earthquakeVelocity structure in the crust beneath the Kyushu areaEvolutionary process of Beppu Bay in central Kyushu, Japan : a quantitative study of the basin-forming process controlled by plate convergence modes
- 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CrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 9772866
- NII論文ID
- 120005756323