Rupture process of the 2016 Kumamoto earthquake in relation to the thermal structure around Aso volcano
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- Material Type
- 記事
- Author/Editor
- Yuji YagiRyo OkuwakiBogdan Enescu
- Publication, Distribution, etc.
- Publication Date
- 2016-07-14
- Publication Date (W3CDTF)
- 2016-07-14
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 68(118)
- Volume
- 68(118)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-016-0492-3
- Persistent ID (NDL)
- info:ndljp/pid/10193195
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 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
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2016-09-08T09:53:02+09:00
- Date Captured (W3CDTF)
- 2016-08-26
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/9963599
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- We constructed the rupture process model for the 2016 Kumamoto, Japan, earthquake from broadband teleseismic body waveforms (P-waves) by using a novel waveform inversion method that takes into account the uncertainty of Green’s function. The estimated source parameters are: seismic moment = 5.1 × 1019 Nm (Mw = 7.1), fault length = 40 km, and fault width = 15 km. The mainshock rupture mainly propagated northeastward from the epicenter, for about 30 km, along an active strike-slip fault. The rupture propagation of the mainshock decelerated and terminated near the southwest side of the Aso volcano; the aftershock activity was low around the northeastern edge of the major slip area. Our results suggest that the rupture process of the mainshock and the distribution of aftershocks were influenced by the high-temperature area around the magma chamber of Mt. Aso
- DOI
- 10.1186/s40623-016-0492-3
- Access Restrictions
- インターネット公開
- Rights (production)
- © 2016 The Author(s).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.
- Related Material (URI)
- Is Referenced By
- Volcanic magma reservoir imaged as a low-density body beneath Aso volcano that terminated thr 2016 Kumamoto earthquake ruptureRemote triggering of seismicity at Japanese volcanoes following the 2016 M7.3 Kumamoto earthquakeSimultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR dataTriggering and decay characteristics of dynamically activated seismicity in Southwest JapanThermal properties of rock core samples and their correlations with other physical properties in the volcanic region surrounding the Aso VolcanoSurface displacements of Aso volcano after the 2016 Kumamoto earthquake based on SAR interferometry: implications for dynamic triggering of earthquake-volcano interactionsEarthquake-induced structural deformations enhance long-term solute fluxes from active volcanic systemsThe influence of pulse-like ground motion caused by the directivity effect on landslide triggeringSpatial and temporal seismic velocity changes on Kyushu Island during the 2016 Kumamoto earthquakeRETRACTED: Coseismic rupturing stopped by Aso volcano during the 2016 <i>M</i> <sub>w</sub> 7.1 Kumamoto earthquake, JapanRETRACTED ARTICLE: Structural features and seismotectonic implications of coseismic surface ruptures produced by the 2016 Mw 7.1 Kumamoto earthquakeImpacts of disaster on the inbound tourism economy in Kyushu, Japan: a demand side analysisChanges in seismicity pattern due to the 2016 Kumamoto earthquake sequence and implications for improving the foreshock traffic-light systemModeling and Forecasting Aftershocks Can Be Improved by Incorporating Rupture Geometry in the ETAS ModelHigh-resolution image on terminus of fault rupture: relationship with volcanic hydrothermal structureRecurrent large earthquakes related with an active fault-volcano system, southwest JapanHorizontal sliding of kilometre-scale hot spring area during the 2016 Kumamoto earthquakeToward automated directivity estimates in earthquake moment tensor inversionMillennium Recurrence Interval of Morphogenic Earthquakes on the Seismogenic Fault Zone That Triggered the 2016 Mw 7.1 Kumamoto Earthquake, Southwest JapanReal-Time GNSS Analysis System REGARD: An Overview and Recent ResultsSeismicity prior to the 2016 Kumamoto earthquakes3-D dynamic rupture simulations of the 2016 Kumamoto, Japan, earthquakeThe 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 earthquakes
- References
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- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 学術機関リポジトリ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CrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10193195
- NAID
- 120005997866