Remote triggering of seismicity at Japanese volcanoes following the 2016 M7.3 Kumamoto earthquake

• 資料種別: 記事
• タイトル: Remote triggering of seismicity at Japanese volcanoes following the 2016 M7.3 Kumamoto earthquake
• 著者・編者: Bogdan Enescu; Kengo Shimojo; Anca Opris
• 出版事項: 日本 : Springer science+business media
• 出版年月日等: 2016-10-20
• 出版年（W3CDTF）: 2016-10-20
• タイトル（掲載誌）: EPS : Earth, Planets and Space
• 巻号年月日等（掲載誌）: 68(165)
• 掲載巻: 68(165)
• 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/s40623-016-0539-5; https://doi.org/10.1186/s40623-016-0539-5
• 国立国会図書館永続的識別子: info:ndljp/pid/10267436; https://dl.ndl.go.jp/pid/10267436
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• 受理日（W3CDTF）: 2017-01-25T12:55:04+09:00
• 保存日（W3CDTF）: 2017-01-13
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• 掲載誌（国立国会図書館永続的識別子）: info:ndljp/pid/9963599; https://dl.ndl.go.jp/pid/9963599
• 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 M[JMA]7.3 Kumamoto earthquake occurred on April 16, 2016, in the western part of Kyushu, at a depth of 12 km, on an active strike-slip fault. Here, we report on a relatively widespread activation of small remote earthquakes, which occurred as far as Hokkaido, detected by analyzing the continuous waveform data recorded at seismic stations all over Japan. Such relatively widespread remote seismicity activation, following a large inland earthquake, has not been reported before for Japan. Our analysis demonstrates that the remote events were triggered dynamically, by the passage of the surface waves from the Kumamoto earthquake. Most of the remotely triggered events in the Tohoku and Hokkaido regions, as well as close to Izu Peninsula, occur at or close to volcanoes, which suggests that the excitation of crustal fluids, by the passage of Rayleigh waves, played an important triggering role. Nevertheless, remote activation in other regions, like Noto Peninsula, occurred away from volcanoes. The relatively large-amplitude Love waves, enhanced by a source directivity effect during the Kumamoto earthquake, may have triggered seismicity on local active faults. The dynamic stresses in the areas where remote activation has been observed range from several kPa to tens of kPa, the thresholds being lower than in previous dynamic triggering cases for Japan; this might relate to a change in the crustal conditions following the 2011 M9.0 Tohoku-oki earthquake, in particular at volcanoes in NE Japan.
• DOI: 10.1186/s40623-016-0539-5; https://doi.org/10.1186/s40623-016-0539-5
• 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: © The Author(s) 2016.; 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）: http://hdl.handle.net/2241/00144454; https://tsukuba.repo.nii.ac.jp/records/39792; http://hdl.handle.net/2433/217628; http://id.ndl.go.jp/digimeta/10267436; https://dl.ndl.go.jp/pid/10267436; http://link.springer.com/content/pdf/10.1186/s40623-016-0539-5.pdf; http://link.springer.com/article/10.1186/s40623-016-0539-5/fulltext.html
• 参照: Triggering and decay characteristics of dynamically activated seismicity in Southwest Japan; https://cir.nii.ac.jp/crid/1050001335857612416; Dynamic Triggering of Earthquakes in Northeast Japan before and after the 2011 M 9.0 Tohoku-Oki Earthquake; https://cir.nii.ac.jp/crid/1050869445406546176; Evaluation of Phenomena Preceding Earthquakes and Earthquake Predictability; https://cir.nii.ac.jp/crid/1390846609814385792
• 参照: Fluid‐driven seismicity activation in northern Nagano region after the 2011 <i>M</i>9.0 Tohoku‐oki earthquake; https://cir.nii.ac.jp/crid/1050282677530712064; Rupture process of the 2016 Kumamoto earthquake in relation with the thermal structure around Aso volcano; https://cir.nii.ac.jp/crid/1050282677536988928; Propagation of an earthquake triggering front from the 2011 Tohoku-Oki earthquake; https://cir.nii.ac.jp/crid/1050282810703024896; Source-Rupture Process of the 2007 Noto Hanto, Japan, Earthquake Estimated by the Joint Inversion of Strong Motion and GPS Data; https://cir.nii.ac.jp/crid/1050564285783286272; Widespread seismicity excitation throughout central Japan following the 2011 M=9.0 Tohoku earthquake and its interpretation by Coulomb stress transfer; https://cir.nii.ac.jp/crid/1360004233288139392; Global patterns of radiated seismic energy and apparent stress; https://cir.nii.ac.jp/crid/1360011144093676672; Mapping pressurized volcanic fluids from induced crustal seismic velocity drops; https://cir.nii.ac.jp/crid/1360283693415694080; The Absence of Remotely Triggered Seismicity in Japan; https://cir.nii.ac.jp/crid/1360292621587090304; Tremors along the Queen Charlotte Margin triggered by large teleseismic earthquakes; https://cir.nii.ac.jp/crid/1360565164505737856; Dynamic Stresses, Coulomb Failure, and Remote Triggering--Corrected; https://cir.nii.ac.jp/crid/1360574094261350272; A new observation of dynamically triggered regional seismicity: Earthquakes in Greece following the August 1999 Izmit, Turkey earthquake; https://cir.nii.ac.jp/crid/1360574094831061504; Dynamic Triggering; https://cir.nii.ac.jp/crid/1361418519426018432; Dynamic triggering of microearthquakes in three geothermal/volcanic regions of California; https://cir.nii.ac.jp/crid/1361699995010619264; The global aftershock zone; https://cir.nii.ac.jp/crid/1361981469875945088; Connecting near‐field and far‐field earthquake triggering to dynamic strain; https://cir.nii.ac.jp/crid/1362544418669839616; Stress perturbations and seismic response associated with the 2011 M9.0 Tohoku‐oki earthquake in and around the Tokai seismic gap, central Japan; https://cir.nii.ac.jp/crid/1362544419242647040; Interference of long-period seismic wavefield observed by the dense Hi-net array in Japan; https://cir.nii.ac.jp/crid/1363107369380756992; Seismicity Remotely Triggered by the Magnitude 7.3 Landers, California, Earthquake; https://cir.nii.ac.jp/crid/1363107370121918080; Remote triggering of tremor along the San Andreas Fault in central California; https://cir.nii.ac.jp/crid/1363388844310596864; SEISMIC TRIGGERING OF ERUPTIONS IN THE FAR FIELD: Volcanoes and Geysers; https://cir.nii.ac.jp/crid/1363388845780611584; Seismic activity near the Moriyoshi-zan volcano in Akita Prefecture, northeastern Japan : implications for geofluid migration and a midcrustal geofluid reservoir; https://cir.nii.ac.jp/crid/2050307417163377792; Remotely-triggered seismicity in the Hakone volcano following the 2011 off the Pacific coast of Tohoku Earthquake; https://cir.nii.ac.jp/crid/2050588892138321536
• 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/
• 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; https://irdb.nii.ac.jp; 雑誌記事索引データベース; https://ndlsearch.ndl.go.jp; Crossref; https://www.crossref.org; CiNii Articles; 科学研究費助成事業データベース; https://kaken.nii.ac.jp/ja
• 書誌ID（NDLBibID）: 10267436; http://id.ndl.go.jp/bib/10267436
• NII論文ID: 120007129288