Seismicity controlled by resistivity structure : the 2016 Kumamoto earthquakes, Kyushu Island, Japan
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DOI[10.1186/s40623-016-0590-2]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
- Koki AizawaHisafumi AsaueKatsuaki Koike
- 出版年月日等
- 2017-01-03
- 出版年（W3CDTF）
- 2017-01-03
- タイトル（掲載誌）
- EPS : Earth, Planets and Space
- 巻号年月日等（掲載誌）
- 69(4)
- 掲載巻
- 69(4)
- 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/s40623-016-0590-2
- 国立国会図書館永続的識別子
- info:ndljp/pid/10319655
- 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（URI）
- 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
- The M JMA 7.3 Kumamoto earthquake that occurred at 1:25 JST on April 16, 2016, not only triggered aftershocks in the vicinity of the epicenter, but also triggered earthquakes that were 50–100 km away from the epicenter of the main shock. The active seismicity can be divided into three regions: (1) the vicinity of the main faults, (2) the northern region of Aso volcano (50 km northeast of the mainshock epicenter), and (3) the regions around three volcanoes, Yufu, Tsurumi, and Garan (100 km northeast of the mainshock epicenter). Notably, the zones between these regions are distinctively seismically inactive. The electric resistivity structure estimated from one-dimensional analysis of the 247 broadband (0.005–3000 s) magnetotelluric and telluric observation sites clearly shows that the earthquakes occurred in resistive regions adjacent to conductive zones or resistive-conductive transition zones. In contrast, seismicity is quite low in electrically conductive zones, which are interpreted as regions of connected fluids. We suggest that the series of the earthquakes was induced by a local accumulated stress and/or fluid supply from conductive zones. Because the relationship between the earthquakes and the resistivity structure is consistent with previous studies, seismic hazard assessment generally can be improved by taking into account the resistivity structure. Following on from the 2016 Kumamoto earthquake series, we suggest that there are two zones that have a relatively high potential of earthquake generation along the western extension of the MTL.
- DOI
- 10.1186/s40623-016-0590-2
- 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
- Creative Commons Attribution 4.0 International
- 関連情報
- Seismicity controlled by resistivity structure: The 2016 Kumamoto earthquakes, Kyushu Island, Japan
- 関連情報（URI）
- 参照
- Prestate of Stress and Fault Behavior During the 2016 Kumamoto Earthquake (<i>M</i>7.3)Potential fluid flow pathways and the geothermal structure of Kuju revealed by azimuthal anisotropic ambient noise tomographyTracking supercritical geothermal fluid distribution from continuous seismic monitoringThree‐Dimensional Electrical Resistivity Distribution Beneath the Beppu–Shimabara Graben With a Focus on Aso Caldera, Southwest Japan Subduction ZoneThe Advancement of Research on Inland Earthquake Generation 2014–2018A 3D electrical resistivity model around the focal zone of the 2017 southern Nagano Prefecture earthquake (MJMA 5.6) : implications for relationship between seismicity and crustal heterogeneityStress and pore fluid pressure control of seismicity rate changes following the 2016 Kumamoto earthquake, JapanThree-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
- An investigation into the remote triggering of the Oita earthquake by the 2016 Mw 7.0 Kumamoto earthquake using full wavefield simulationCrustal structure and fluid distribution beneath the southern part of the <scp>H</scp>idaka collision zone revealed by 3‐<scp>D</scp> electrical resistivity modelingSpatial heterogeneities in tectonic stress in Kyushu, Japan and their relation to a major shear zoneMagnetotelluric observations around the focal region of the 2007 Noto HantoEarthquake (Mj6.9), Central JapanIncreased radon-222 in soil gas because of cumulative seismicity at active faultsSource rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion dataCrustal magma pathway beneath Aso caldera inferred from 3-D electrical resistivity structureElectrical characterization of the North Anatolian Fault Zone underneath the Marmara Sea, Turkey by ocean bottom magnetotelluricsOn the Berdichevsky averageA large intraplate earthquake triggered by latent magmatismOccam's inversion; a practical algorithm for generating smooth models from electromagnetic sounding dataFluid and deformation regime of an advancing subduction system at Marlborough, New ZealandGas pathways and remotely triggered earthquakes beneath Mount Fuji, JapanCrustal velocity field of southwest Japan: Subduction and arc‐arc collisionFluid generation and pathways beneath an active compressional orogen, the New Zealand Southern Alps, inferred from magnetotelluric dataSyntheses of the regional stress fields of the Japanese islandsApplication of Magnetotelluric (MT) Resistivity to Imaging of Regional Three-Dimensional Geologic Structures and Groundwater SystemsEarthquake doublet in an active shear zone, southwest Japan: Constraints from geophysical and geochemical findingsMagnetotelluric imaging of the Median Tectonic Line in western Shikoku, southwest Japan: Implications of the fault-related low-resistivity zoneVolcanic and structural history of the Hohi volcanic zone, central Kyushu, JapanMagnetotelluric resistivity modeling for 3D characterization of geothermal reservoirs in the Western side of Mt. Aso, SW JapanStress, strain rate and anisotropy in Kyushu, JapanA fault‐zone conductor beneath a compressional inversion zone, northeastern Honshu, JapanA model for the motion of the Philippine Sea Plate consistent with NUVEL‐1 and geological dataModEM: A modular system for inversion of electromagnetic geophysical dataA model with rigid rotations and slip deficits for the GPS-derived velocity field in Southwest JapanWater-weakened lower crust and its role in the concentrated deformation in the Japanese IslandsElectrical conductivity anomalies beneath the Western Sea of Kyushu, JapanMagnetotelluric imaging of the fault rupture area of the 1999 İzmit (Turkey) earthquakeResistivity structure of a seismic gap along the Atotsugawa Fault, JapanThe magnetotelluric phase tensorAnalysis of rotational invariants of the magnetotelluric impedance tensorMagmatic unrest beneath Mammoth Mountain, CaliforniaResistivity structure underneath the Pamir and Southern Tian ShanMagnetotellurics with a remote magnetic referenceMagnetotelluric imaging of fluids in intraplate earthquake zones, NE Japan Back ArcInternal structure of the San Andreas fault at Parkfield, CaliforniaElectromagnetic heterogeneity of the seismogenic region of 1962 M6.5 Northern Miyagi Earthquake, northeastern JapanA new hypothesis for the deep subsurface structures near the Bhuj 2001 earthquake (Mw 7.6) hypocentre zone and its tectonic implicationsA deep crustal fluid channel into the San Andreas Fault system near Parkfield, CaliforniaSeismotectonics of the Median Tectonic Line in southwest Japan: Implications for coupling among major fault systemsRelation between electrical resistivity and earthquake generation in the crust of West Anatolia, TurkeyThe static stress change triggering model: Constraints from two southern California aftershock sequencesResistivity structure around the focal area of the 2004 Rumoi-Nanbu earthquake (M 6.1), northern Hokkaido, JapanAsperity along the North Anatolian Fault imaged by magnetotellurics at Düzce, TurkeyMagnetotelluric transect across the Niigata‐Kobe Tectonic Zone, central Japan: A clear correlation between strain accumulation and resistivity structureBounded influence magnetotelluric response function estimationTectonics of an arc-arc junction: an example from Kyushu Island at the junction of the Southwest Japan Arc and the Ryukyu ArcWSINV3DMT: Vertical magnetic field transfer function inversion and parallel implementationEnigmatic, highly active left-lateral shear zone in southwest Japan explained by aseismic ridge collisionHistory of basin formation and tectonic evolution at the termination of a large transcurrent fault system: deformation mode of central Kyushu, JapanaＭＴ法による活断層深部の破砕構造解析Resistivity imaging across the source region of the 2004 Mid-Niigata Prefecture earthquake (M6.8), central JapanLateral inhomogeneity deduced from 3-D magnetotelluric modeling around the hypocentral area of the 1984Western Nagano Prefecture earthquake, central JapanResistivity structure in the western part of the fault rupture zone associated with the 1999 İzmit earthquake and its seismogenic implication布田川‐日奈久断層帯の深部比抵抗構造のイメージングと微小地震分布からの考察Electrical conductivity structures estimated by thin sheet inversion, with special attention to the Beppu-Shimabara graben in central Kyushu, JapanConductivity distribution and seismicity in the northeastern Japan ArcSubsurface structure and faulting of the Median Tectonic Line, southwest Japan inferred from GPS velocity fieldMagnetotelluric and temperature monitoring after the 2011 sub-Plinian eruptions of Shinmoe-dake volcanoA 3-D electrical resistivity model beneath the focal zone of the 2008 Iwate-Miyagi Nairiku earthquake (M 7.2)Velocity 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 modesThree-dimensional magnetotelluric imaging of crustal fluids and seismicity around Naruko volcano, NE Japan
- 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学術機関リポジトリデータベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 10319655
- NII論文ID
- 120006360155