| DOI: | 10.1016/j.tecto.2021.228772
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| 论文题名: | Corrigendum to Enhancement of interplate coupling in adjacent segments after recent megathrust earthquakes. Tectonophysics 801 (2021) 228719. https://doi.org/10.1016/j.tecto.2021.228719 (Tectonophysics (2021) 801, (S0040195121000032), (10.1016/j.tecto.2021.228719)) |
| 作者: | Yuzariyadi M.; Heki K.
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| 刊名: | Tectonophysics
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| ISSN: | 00401951
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| 出版年: | 2021
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| 卷: | 805 | | 语种: | 英语
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| 英文关键词: | Clupeidae
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| 英文摘要: | The authors regret to inform that an important information was missing in the article. This corrigendum aims to acknowledge those who installed and operated GNSS stations in Sumatra, South and Middle America. Also, there are several additional information/changes to avoid confusion. The changes are shown below. The second paragraph of subsection 2.1: “In Sumatra, we analyzed the data from the Sumatran GPS Array (SuGAr) stations provided by Earth Observatory of Singapore (EOS) and Indonesian Institute of Sciences (LIPI) via Bandung Institute of Technology (Ardika et al., 2015). These data are processed using the GAMIT 10.5 to obtain daily solutions (Herring et al., 2018). For the South and Middle American data, we analyzed the Precise Point Positioning (PPP) solutions available from the Nevada Geodetic Laboratory at geodesy.unr.edu (Blewitt et al., 2018) and partly from Jet Propulsion Laboratory at sideshow.jpl.nasa.gov/post/series.html. The GNSS data in South America are from ENS/CNRS and Centro Sismologico Nacional of Chile (CSN) (Báez et al., 2018). For Middle America, the GNSS data are from the Trans-boundary, Land and Atmosphere Long-term Observational and Collaborative Network (TLALOCNet) (Cabral-Cano et al., 2018)”. The first paragraph of subsection 4.3 (the fourth and fifth sentences): “Ruiz et al. (2016) and Melnick et al. (2017) reported a postseismic increase of the landward velocities of stations located to the north of the rupture. Melnick et al. (2017) suggested that such enhanced coupling may have triggered the occurrence of the 2015 Illapel earthquake (Mw 8.3) to the north of the 2010 rupture”. In the sixth sentence of the second paragraph, the text should be: “the stations in Fig. 8b and c showing enhanced landward velocities, including CNBA, suffer from data gaps up to two years in the Nevada Geodetic Laboratory database”. The fifth paragraph of subsection 5.6 (the first sentence): “The dashed line in Fig. 17c has the slope of 6.1 × 103 m yr−1, which corresponds to 1.93 × 10−4 m s−1”. The Figures were made using free GMT (Generic Mapping Tools) software (Wessel and Smith, 1991). The GEONET F3 solutions were downloaded from terras.gsi.go.jp. We used a computer code for the space-time ETAS model and stochastic declustering from http://bemlar.ism.ac.jp/zhuang/software.html. We thank Kei Katsumata, Hokkaido University, for discussion on the change in seismicity associated with the 2011 Tohoku-oki earthquake. The authors would like to apologise for any inconvenience caused by this. © 2021 The Author(s) |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/170934
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| Appears in Collections: | 气候变化与战略
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作者单位: | Department of Natural History Sci, Hokkaido University, N10 W8, Kita-ku, Sapporo, Japan
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| Recommended Citation: | |
Yuzariyadi M.,Heki K.. Corrigendum to Enhancement of interplate coupling in adjacent segments after recent megathrust earthquakes. Tectonophysics 801 (2021) 228719. https://doi.org/10.1016/j.tecto.2021.228719 (Tectonophysics (2021) 801, (S0040195121000032), (10.1016/j.tecto.2021.228719))[J]. Tectonophysics,2021-01-01,805
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