In the original article, there were mistakes in Figure 1B and Figure 13. In these figures, there were wrong focal mechanisms of VLFE, which contradicted with those in Figure 1A. The corrected Figure 1B and Figure 13 appear below.
FIGURE 1
FIGURE 13

Schematic scenario of the possible process for the SSE with ocean loading (A) during model A-1, (B) during model A-2+, and (C) termination of the SSE. Representative focal mechanism of VLFE is obtained from
As an additional explanation for Figure 1B, “the focal depths of the fault models A-1 and A-2+ are assumed to be consistent with VLFE because it is practically difficult to determine the focal depth precisely from only the two volumetric strain data at boreholes (C0002 and C0010) by using the simplified green’s function.”
The authors apologize for these errors and state that they do not change the scientific conclusions of the article in any way. The original article has been updated.
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All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.
References
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AriyoshiK.IinumaT.NakanoM.KimuraT.ArakiE.MachidaY.et al (2021). Characteristics of Slow Slip Event in March 2020 Revealed from Borehole and DONET Observatories. Front. Earth Sci.8, 600793. 10.3389/feart.2020.600793
2
NakanoM.HoriT.ArakiE.KodairaS.IdeS. (2018). Shallow Very-Low-Frequency Earthquakes Accompany Slow Slip Events in the Nankai Subduction Zone. Nat. Commun.9, 984. 10.1038/s41467-018-03431-5
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KinoshitaM.BeckerK.ToczkoS.EdgingtonJ.KimuraT.MachidaY.et al (2018). “Expedition 380 Methods,” in The Expedition 380 Scientists, NanTroSEIZE Stage 3: Frontal Thrust Long-Term Borehole Monitoring System (LTBMS). Proceedings of the International Ocean Discovery Program. Editors BeckerK.KinoshitaM.ToczkoS. (College Station, TX: International Ocean Discovery Program), 380. 10.14379/iodp.proc.380.102.2018
Summary
Keywords
slow slip event, slow earthquake, kuroshio meander, nankai trough, ocean modeling
Citation
Ariyoshi K, Kimura T, Miyazawa Y, Varlamov S, Iinuma T, Nagano A, Gomberg J, Araki E, Miyama T, Sueki K, Yada S, Hori T, Takahashi N and Kodaira S (2021) Corrigendum: Precise Monitoring of Pore Pressure at Boreholes Around Nankai Trough Toward Early Detecting Crustal Deformation. Front. Earth Sci. 9:770719. doi: 10.3389/feart.2021.770719
Received
04 September 2021
Accepted
16 September 2021
Published
30 September 2021
Volume
9 - 2021
Edited and reviewed by
Sergey V. Samsonov, Department of Natural Resources, Canada
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Copyright
© 2021 Ariyoshi, Kimura, Miyazawa, Varlamov, Iinuma, Nagano, Gomberg, Araki, Miyama, Sueki, Yada, Hori, Takahashi and Kodaira.
This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice.
*Correspondence: Keisuke Ariyoshi, ariyoshi@jamstec.go.jp
This article was submitted to Solid Earth Geophysics, a section of the journal Frontiers in Earth Science
Disclaimer
All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.