Source rupture processes of the 2016 Kumamoto, Japan, earthquakes estimated from strong-motion waveforms
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DOI[10.1186/s40623-016-0536-8]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Hisahiko KuboWataru SuzukiShin Aoi
- Publication, Distribution, etc.
- Publication Date
- 2016-10-03
- Publication Date (W3CDTF)
- 2016-10-03
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 68(161)
- Volume
- 68(161)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-016-0536-8
- Persistent ID (NDL)
- info:ndljp/pid/10267432
- 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)
- 2017-01-25T12:55:04+09:00
- Date Captured (W3CDTF)
- 2017-01-13
- 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.
- The detailed source rupture process of the M 7.3 event (April 16, 2016, 01:25, JST) of the 2016 Kumamoto, Japan, earthquakes was derived from strong-motion waveforms using multiple-time-window linear waveform inversion. Based on the observations of surface ruptures, the spatial distribution of aftershocks, and the geodetic data, a realistic curved fault model was developed for source-process analysis of this event. The seismic moment and maximum slip were estimated as 5.5 × 1019 Nm (M w 7.1) and 3.8 m, respectively. The source model of the M 7.3 event had two significant ruptures. One rupture propagated toward the northeastern shallow region at 4 s after rupture initiation and continued with large slips to approximately 16 s. This rupture caused a large slip region 10–30 km northeast of the hypocenter that reached the caldera of Mt. Aso. Another rupture propagated toward the surface from the hypocenter at 2–6 s and then propagated toward the northeast along the near surface at 6–10 s. A comparison with the result of using a single fault plane model demonstrated that the use of the curved fault model led to improved waveform fit at the stations south of the fault. The source process of the M 6.5 event (April 14, 2016, 21:26, JST) was also estimated. In the source model obtained for the M 6.5 event, the seismic moment was 1.7 × 1018 Nm (M w 6.1), and the rupture with large slips propagated from the hypocenter to the surface along the north-northeast direction at 1–6 s. The results in this study are consistent with observations of the surface ruptures.
- DOI
- 10.1186/s40623-016-0536-8
- 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
- Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR dataThe Origin of Large, Long‐Period Near‐Fault Ground Velocities During Surface‐Breaking Strike‐Slip EarthquakesThe influence of pulse-like ground motion caused by the directivity effect on landslide triggeringRETRACTED ARTICLE: Structural features and seismotectonic implications of coseismic surface ruptures produced by the 2016 Mw 7.1 Kumamoto earthquakeConstraint 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 rotationStrong ground motion simulations of the 2016 Kumamoto earthquakes using corrected empirical Green’s functions: methods and results for ESG6 blind prediction Steps 2 and 3 with improved parametersHigh-resolution image on terminus of fault rupture: relationship with volcanic hydrothermal structureRecurrent large earthquakes related with an active fault-volcano system, southwest JapanToward automated directivity estimates in earthquake moment tensor inversionNumerical Shake Prediction for Earthquake Early Warning Incorporating Heterogeneous Attenuation Structure: The Case of the 2016 Kumamoto EarthquakeStrain energy released by earthquake faulting with random slip componentsToo-Late Warnings by Estimating Mw: Earthquake Early Warning in the Near-Fault Region2016年熊本地震の震源近傍の地震被害と震源モデルの構築2016年熊本地震最大前震 (Mj6.5) のKiK-net益城観測点における大加速度振幅の要因分析及び基盤地震動の推定九州地域の震源特性・不均質伝播経路特性・サイト増幅特性の推定強震記録や木造被害分布に基づく，M7クラスの内陸地殻内地震で震度7が発生しやすい場所の整理臨時地震観測に基づく2016年熊本地震の前震による高速道路盛土の被災地点での強震動の評価2016年熊本地震における大振幅速度パルスの解釈と断層近傍地震動に対する浅部・深部断層破壊の影響CONSTRUCTION OF GROUND MOTION EVALUATION MODELS USING SUPERVISED MACHINE LEARNING BASED ON STRONG MOTION DATABASE異なる手法による日本の地殻内地震の短周期レベルの比較地表地震断層近傍における永久変位を含む長周期成分の地震動評価のための震源モデルの設定方法2016年熊本地震の震源近傍における強震動の再現解析と空間分布不均質震源断層モデルのすべり角のばらつき2016年熊本地震と布田川断層，地震地質災害強震動データベースに基づく機械学習による地震動評価モデルの構築内陸で発生した歴史地震の震度データに基づく断層モデルの構築Real-time automatic uncertainty estimation of coseismic single rectangular fault model using GNSS data3-D dynamic rupture simulations of the 2016 Kumamoto, Japan, earthquakeSource location and mechanism analysis of an earthquake triggered by the 2016 Kumamoto, southwestern Japan, earthquakeSlip-partitioned surface ruptures for the Mw 7.0 16 April 2016 Kumamoto, Japan, earthquakeCharacteristics of secondary-ruptured faults in the Aso Caldera triggered by the 2016 Mw 7.0 Kumamoto earthquake
- 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雑誌記事索引データベースCrossrefCiNii ArticlesCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10267432
- NAID
- 120005997861
- Summary, etc.
- We determined the sulfation patterns and the amount of chondroitin sulfate in several tissues of the diamond squid, <I>Thysanoteuthis rhombus</I>. Every tissue contained the highly-sulfated E type of chondroitin. The arms, skin, and fin had non-sulfated chondroitin as the homogenous polymer. The skin and fin possessed larger amounts of chondroitin sulfate per unit of weight than the other tissues.
- DOI
- 10.1271/bbb.90037
- Related Material (URI)
- Is Referenced By
- Quantitative, compositional, and immunohistochemical analyses of chondroitin sulfate, dermatan sulfate, and hyaluronan in internal organs of deer (Cervus nippon centralis and C. n. yesoensis) and cattle (Bos taurus)Depolymerization of sulfated polysaccharides under hydrothermal conditionsFacile analysis of contents and compositions of the chondroitin sulfate/dermatan sulfate hybrid chain in shark and ray tissues生化学機能を持つコンドロイチン硫酸オリゴ糖の精密化学合成
- References
- Antibodies to Three Chondroitin Sulfate-Containing Proteoglycans in Squid Skin Recognize Hexa- or Longer Chondroitin Oligosaccharides as Major Antigenic DeterminantsAnalysis of the acid polysaccharides from squid cranial cartilage and examination of a novel polysaccharideHeterogeneity of the Chondroitin Sulfate Portion of Phosphacan/6B4 Proteoglycan Regulates Its Binding Affinity for Pleiotrophin/Heparin Binding Growth-associated MoleculeTwo squid skin proteoglycans each containing chondroitin sulfates with different sulfation patternsChondroitin Sulfate Perlecan Enhances Collagen Fibril FormationThe reaction of carbazole with carbohydratesAnalysis of unsaturated disaccharides from glycosaminoglycuronan by high-performance liquid chromatographyIsolation and chemical study of the glycosaminoglycans from squid corneaChondroitin Sulfate Characterized by the E-disaccharide Unit Is a Potent Inhibitor of Herpes Simplex Virus Infectivity and Provides the Virus Binding Sites on gro2C CellsAppican, the Proteoglycan Form of the Amyloid Precursor Protein, Contains Chondroitin Sulfate E in the Repeating Disaccharide Region and 4-O-Sulfated Galactose in the Linkage RegionChondroitin-protein complex from squid skinComparison of the glycosaminoglycans isolated from the skin and head cartilage of Gould's arrow squid (Nototodarus gouldi)Distribution of sulfated mucopolysaccharides in invertebrates.Importance of GlcUAβ1-3GalNAc(4S,6S) in chondroitin sulfate E for t-PA- and u-PA-mediated Glu-plasminogen activationThe engelbreth-holm-swarm mouse tumor produces undersulfated heparan sulfate and oversulfated galactosaminoglycansOversulfated Chondroitin/Dermatan Sulfates Containing GlcAβ1/IdoAα1–3GalNAc(4,6-O-disulfate) Interact with L- and P-selectin and ChemokinesNeuronal Cell Adhesion, Mediated by the Heparin-binding Neuroregulatory Factor Midkine, Is Specifically Inhibited by Chondroitin Sulfate EIsolation and Structural Determination of Novel Sulfated Hexasaccharides from Squid Cartilage Chondroitin Sulfate E That Exhibits Neuroregulatory ActivitiesDomain Structure of Chondroitin Sulfate E Octasaccharides Binding to Type V Collagen
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- Japan Link Center雑誌記事索引データベースCrossrefCiNii ArticlesCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10267432
- NAID
- 10027542632