Detection of small crustal deformation caused by slow slip events in southwest Japan using GNSS and tremor data
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- Material Type
- 記事
- Author/Editor
- Megumi FujitaTakuya NishimuraShin’ichi Miyazaki
- Publication, Distribution, etc.
- Publication Date
- 2019-09-06
- Publication Date (W3CDTF)
- 2019-09-06
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 71(96)
- Volume
- 71(96)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-019-1075-x
- Persistent ID (NDL)
- info:ndljp/pid/11377521
- 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)
- 2019-10-28T20:45:15+09:00
- Date Captured (W3CDTF)
- 2019-10-28
- 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/11245705
- 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 stacked daily Global Navigation Satellite System (GNSS) displacement increments in southwest Japan to detect the cumulative crustal deformation accompanying non-volcanic low-frequency tremors from April 1, 2004 to December 31, 2009, which are difficult to identify for individual slow slip events (SSEs). We successfully detected the crustal deformation associated with the tectonic stress releases coincident with tremor activity, which was larger than that caused by short-term SSEs detected in previous studies. To investigate the characteristics of the detected crustal deformation, we estimated the parameters of a rectangular fault model in segments along the Nankai Trough using a non-linear inversion method. Consequently, we obtained results that were concordant with those of previous studies and positive linear correlations between the moment and tremor energy in some segments. The linear regression slopes differed, reflecting the fact that the excitation efficiency of the tremors resulting from slow slip was different for each segment. Our results suggest that tremor activity serves as a proxy for SSEs, reflecting the different characteristics of SSEs in segments.
- DOI
- 10.1186/s40623-019-1075-x
- Access Restrictions
- インターネット公開
- Rights (production)
- © The Author(s) 2019. 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
- Slow Slip Events in the Kanto and Tokai Regions of Central Japan Detected Using Global Navigation Satellite System Data During 1994–2020Imaging evolution of Cascadia slow-slip event using high-rate GPS<i>l</i> <sub>1</sub> Trend Filtering‐Based Detection of Short‐Term Slow Slip Events: Application to a GNSS Array in Southwest Japan
- 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CrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11377521
- NAID
- 120006799253