Magnitude-frequency distribution of volcanic explosion earthquakes
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DOI[10.1186/s40623-016-0505-2]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Takeshi NishimuraMasato IguchiMohammad Hendrasto
- Publication, Distribution, etc.
- Publication Date
- 2016-07-20
- Publication Date (W3CDTF)
- 2016-07-20
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 68(125)
- Volume
- 68(125)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-016-0505-2
- Persistent ID (NDL)
- info:ndljp/pid/10193202
- 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.
- Magnitude–frequency distributions of volcanic explosion earthquakes that are associated with occurrences of vulcanian and strombolian eruptions, or gas burst activity, are examined at six active volcanoes. The magnitude–frequency distribution at Suwanosejima volcano, Japan, shows a power-law distribution, which implies self-similarity in the system, as is often observed in statistical characteristics of tectonic and volcanic earthquakes. On the other hand, the magnitude–frequency distributions at five other volcanoes, Sakurajima and Tokachi-dake in Japan, Semeru and Lokon in Indonesia, and Stromboli in Italy, are well explained by exponential distributions. The statistical features are considered to reflect source size, as characterized by a volcanic conduit or chamber. Earthquake generation processes associated with vulcanian, strombolian and gas burst events are different from those of eruptions ejecting large amounts of pyroclasts, since the magnitude–frequency distribution of the volcanic explosivity index is generally explained by the power law.Nishimura, T., Iguchi, M., Hendrasto, M. et al. Correction to: Magnitude–frequency distribution of volcanic explosion earthquakes. Earth Planets Space 69, 143 (2017).
- DOI
- 10.1186/s40623-016-0505-2
- 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 eruption volume flux estimations from very long period infrasound signalsRheological behavior of water-ash mixtures from Sakurajima and Ontake volcanoes: implications for lahar flow dynamicsAnalyzing the continuous volcanic tremors detected during the 2015 phreatic eruption of the Hakone volcano
- References
- Scaling law of volcanic explosion earthquakeMechanism of explosive eruption revealed by geophysical observations at the Sakurajima, Suwanosejima and Semeru volcanoesMonitoring volcanic activity using correlation patterns between infrasound and ground motionMicrotremors and volcanic explosions at Stromboli — Part 2Mechanism of small vulcanian eruptions at Suwanosejima volcano, Japan, as inferred from precursor inflations and tremor signalsLamb pulse observed in natureThe source of explosive eruptions of Sakurajima volcano, JapanDeep volcanic tremor and magma ascent mechanism under Kilauea, HawaiiTime constraints for modeling source dynamics of volcanic explosions at StromboliSeismic and acoustic observations at Mount Erebus Volcano, Ross Island, Antarctica, 1994–1998Volcanic tremor during eruptions: Temporal characteristics, scaling and constraints on conduit size and processesDuration‐amplitude distribution of volcanic tremorHighlights from a seismic broadband array on Stromboli VolcanoAnalysis of seismic body waves excited by the Mount St. Helens eruption of May 18, 1980The volcanic explosivity index (VEI) an estimate of explosive magnitude for historical volcanismSource mechanisms of volcanic explosion earthquakes: single force and implosive sourcesSource mechanisms of explosions at Stromboli Volcano, Italy, determined from moment‐tensor inversions of very‐long‐period dataTerrestrial Volcanism in Space and TimeVulcanian eruptions with dominant single force components observed during the Asama 2004 volcanic activity in Japan
- 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 Articles科学研究費助成事業データベースCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10193202
- NAID
- 120005997906