Spatiotemporal Variations of Intermediate‐Depth Earthquakes Before and After 2011 Tohoku Earthquake Revealed by a Template Matching Catalog
Abstract
We investigate spatiotemporal changes of intermediate-depth earthquakes in the double seismic zone beneath Central and Northeastern Japan before and after the 2011 magnitude 9 Tohoku earthquake. We build a template-matching catalog 1 year before and 1 year after the Tohoku earthquake using Hi-net recordings. The new catalog has a six-fold increase in earthquakes compared to the Japan Meteorological Agency catalog. Our results show no significant change in the intermediate-depth earthquake rate prior to the Tohoku earthquake, but a clear increase in both planes following the Tohoku earthquake. The regions with increased intermediate-depth earthquake activity and the post-seismic slips following the Tohoku earthquake are spatially separate and complementary with each other. Aftershock productivity of intermediate-depth earthquakes increased in both planes following the Tohoku earthquake. Overall, aftershock productivity of the upper plane is higher than the lower plane, likely indicating that stress environments and physical mechanisms of intermediate-depth earthquakes in the two planes are distinct.
Copyright and License
© 2023 The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited and is not used for commercial purposes.
Acknowledgement
We thank Takeshi Iinuma for sharing the coseismic and postseismic slip models of the Tohoku earthquake. The manuscript benefitted from comments from Jiancang Zhuang, Brent Delbridge, and Shanna Chu. This study used the Bridges2 GPU cluster in the Extreme Science and Engineering Discovery Environment, which is supported by National Science Foundation (NSF, Grant OCI-1053575). Q. Z. and Z. P. were supported by an NSF Grant EAR-1925965, and Y.W. was supported by an NSF Grant EAR-1925920.
Data Availability
The newly built earthquake catalog in this study is publicly available at Zhai (2023). The Hi-net seismic waveforms (National Research Institute for Earth Science and Disaster Resilience, 2019) are publicly available at https://hinetwww11.bosai.go.jp/auth/?LANG=. The JMA earthquake catalog (Tamaribuchi et al., 2016; Ueno, 2002) is publicly available at https://www.data.jma.go.jp/svd/eqev/data/bulletin. The Hi-net seismic waveforms are downloaded using HinetPy (Tian, 2021), publicly available under the MIT license at https://github.com/seisman/HinetPy. The earthquake detection is performed using the EQcorrscan (Chamberlain et al., 2017, 2020), publicly available under the LGPL GNU license at https://github.com/eqcorrscan/EQcorrscan, and the Fast Matched Filter (FMF) (Beaucé et al., 2017), publicly available under the GPL-3.0 license at https://github.com/beridel/fast_matched_filter. All links were last accessed in September 2023.
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Additional details
- ISSN
- 1944-8007
- National Science Foundation
- OCI‐1053575
- National Science Foundation
- EAR‐1925965
- National Science Foundation
- EAR‐1925920
- Caltech groups
- Seismological Laboratory