A long source area of the 1906 Colombia–Ecuador earthquake estimated from observed tsunami waveforms

• 資料種別: 記事
• タイトル: A long source area of the 1906 Colombia–Ecuador earthquake estimated from observed tsunami waveforms
• 著者・編者: Yusuke Yamanaka; Yuichiro Tanioka; Takahiro Shiina
• 出版事項: 日本 : Springer Nature
• 出版年月日等: 2017-12-06
• 出版年（W3CDTF）: 2017-12-06
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 69(163)
• 掲載巻: 69(163)
• 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/s40623-017-0750-z; https://doi.org/10.1186/s40623-017-0750-z
• 国立国会図書館永続的識別子: info:ndljp/pid/11002689; https://dl.ndl.go.jp/pid/11002689
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• 収集根拠: オンライン資料収集制度
• 受理日（W3CDTF）: 2017-12-14T17:18:17+09:00
• 保存日（W3CDTF）: 2017-12-13
• 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
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• 掲載誌（URI）: https://earth-planets-space.springeropen.com/articles
• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/10319651; https://dl.ndl.go.jp/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; https://dl.ndl.go.jp

• 要約等: The 1906 Colombia-Ecuador earthquake induced both strong seismic motions and a tsunami, the most destructive earthquake in the history of the Colombia-Ecuador subduction zone. The tsunami propagated across the Pacific Ocean, and its waveforms were observed at tide gauge stations in countries including Panama, Japan, and the USA. This study conducted slip inverse analysis for the 1906 earthquake using these waveforms. A digital dataset of observed tsunami waveforms at the Naos Island (Panama) and Honolulu (USA) tide gauge stations, where the tsunami was clearly observed, was first produced by consulting documents. Next, the two waveforms were applied in an inverse analysis as the target waveform. The results of this analysis indicated that the moment magnitude of the 1906 earthquake ranged from 8.3 to 8.6. Moreover, the dominant slip occurred in the northern part of the assumed source region near the coast of Colombia, where little significant seismicity has occurred, rather than in the southern part. The results also indicated that the source area, with significant slip, covered a long distance, including the southern, central, and northern parts of the region.
• DOI: 10.1186/s40623-017-0750-z; https://doi.org/10.1186/s40623-017-0750-z
• 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（URI）: https://hdl.handle.net/2115/68290; http://id.ndl.go.jp/digimeta/11002689; https://dl.ndl.go.jp/pid/11002689; http://link.springer.com/content/pdf/10.1186/s40623-017-0750-z.pdf; http://link.springer.com/article/10.1186/s40623-017-0750-z/fulltext.html; http://hdl.handle.net/2115/68290
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• 参照: Traveltime delay and initial phase reversal of distant tsunamis coupled with the self‐gravitating elastic Earth; https://cir.nii.ac.jp/crid/1360002214348554112; Fault size and depth extent of the Ecuador earthquake (<i>M_w</i> 7.8) of 16 April 2016 from teleseismic and tsunami data; https://cir.nii.ac.jp/crid/1360011145278428928; New, improved version of generic mapping tools released; https://cir.nii.ac.jp/crid/1360292617909532032; Global Sea Floor Topography from Satellite Altimetry and Ship Depth Soundings; https://cir.nii.ac.jp/crid/1360292617911557120; An updated digital model of plate boundaries; https://cir.nii.ac.jp/crid/1360292617913680896; Surface deformation due to shear and tensile faults in a half-space; https://cir.nii.ac.jp/crid/1360292621388170624; The seismic coupling of subduction zones revisited; https://cir.nii.ac.jp/crid/1360292621475497728; Preliminary reference Earth model; https://cir.nii.ac.jp/crid/1360574092885172608; Determination of earthquake source parameters from waveform data for studies of global and regional seismicity; https://cir.nii.ac.jp/crid/1360574092892069120; The energy release in great earthquakes; https://cir.nii.ac.jp/crid/1360855567862148224; The global CMT project 2004–2010: Centroid-moment tensors for 13,017 earthquakes; https://cir.nii.ac.jp/crid/1360855567862858240; Global Bathymetry and Elevation Data at 30 Arc Seconds Resolution: SRTM30_PLUS; https://cir.nii.ac.jp/crid/1360855567868940928; Secular seismic energy release in the circum-Pacific belt; https://cir.nii.ac.jp/crid/1360855568535911936; Depth‐dependent rupture mode along the Ecuador‐Colombia subduction zone; https://cir.nii.ac.jp/crid/1360855569550873216; Distribution of discrete seismic asperities and aseismic slip along the Ecuadorian megathrust; https://cir.nii.ac.jp/crid/1360855571497868160; Use of the mantle magnitudeM m for the reassessment of the moment of historical earthquakes; https://cir.nii.ac.jp/crid/1361137043881762304; Recent crustal deformation and the earthquake cycle along the Ecuador–Colombia subduction zone; https://cir.nii.ac.jp/crid/1361137045972271232; The 16 April 2016, M7.8 (M7.5) Ecuador earthquake: A quasi-repeat of the 1942 M7.5 earthquake and partial re-rupture of the 1906 M8.6 Colombia–Ecuador earthquake; https://cir.nii.ac.jp/crid/1361418520389701760; A revised tsunami source model for the 1707 Hoei earthquake and simulation of tsunami inundation of Ryujin Lake, Kyushu, Japan; https://cir.nii.ac.jp/crid/1361418520914994048; Slab1.0: A three‐dimensional model of global subduction zone geometries; https://cir.nii.ac.jp/crid/1361699993445708032; Size of great earthquakes of 1837–1974 inferred from tsunami data; https://cir.nii.ac.jp/crid/1361699995623074304; Modelling of Coulomb stress changes during the great (Mw = 8.8) 1906 Colombia-Ecuador earthquake; https://cir.nii.ac.jp/crid/1361981468641110784; Historical 1942 Ecuador and 1942 Peru subduction earthquakes and earthquake cycles along Colombia-Ecuador and Peru subduction segments; https://cir.nii.ac.jp/crid/1362262945431370496; Dispersion and nonlinear effects in the 2011 Tohoku‐Oki earthquake tsunami; https://cir.nii.ac.jp/crid/1362262945438157184; The rupture process of the Great 1979 Colombia Earthquake: Evidence for the asperity model; https://cir.nii.ac.jp/crid/1362262945880922112; Tsunami generation by horizontal displacement of ocean bottom; https://cir.nii.ac.jp/crid/1362544419007623040; Use of long-period surface waves for rapid determination of earthquake-source parameters; https://cir.nii.ac.jp/crid/1363107370071479808; Rupture zones of large South American earthquakes and some predictions; https://cir.nii.ac.jp/crid/1363670319781208320; 津波波形から推定した詳細な2003年十勝沖地震のすべり量分布; https://cir.nii.ac.jp/crid/1390282679282154496; Global Historical Tsunami Database; https://cir.nii.ac.jp/crid/1881146593277710336
• 連携機関・データベース: 国立情報学研究所 : CiNii Research; https://cir.nii.ac.jp/
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• 書誌ID（NDLBibID）: 11002689; http://id.ndl.go.jp/bib/11002689
• NII論文ID: 120006383816