Natural Hazards and Earth System Sciences
Natural Hazards and Earth System Sciences
NHESS
Articles | Volume 20, issue 12
Articles | Volume 20, issue 12
https://doi.org/10.5194/nhess-20-3333-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-20-3333-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 12
Research article
 | 
09 Dec 2020
Research article |  | 09 Dec 2020

Spatiotemporal changes of seismicity rate during earthquakes

Chieh-Hung Chen, Yang-Yi Sun, Strong Wen, Peng Han, Li-Ching Lin, Huaizhong Yu, Xuemin Zhang, Yongxin Gao, Chi-Chia Tang, Cheng-Horng Lin, and Jann-Yenq Liu

Viewed

Total article views: 1,683 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,122 511 50 1,683 196 54 44
  • HTML: 1,122
  • PDF: 511
  • XML: 50
  • Total: 1,683
  • Supplement: 196
  • BibTeX: 54
  • EndNote: 44
Views and downloads (calculated since 24 Feb 2020)
Cumulative views and downloads (calculated since 24 Feb 2020)

Viewed (geographical distribution)

Total article views: 1,683 (including HTML, PDF, and XML) Thereof 1,556 with geography defined and 127 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Download
Short summary
Scientists demystify stress changes before mainshocks and utilize the foreshocks as an indicator. We investigate changes in seismicity far from mainshocks by using tens of thousands of M ≥ 2 quakes for 10 years in Taiwan and Japan. The results show that wide areas exhibit increased seismicity occurring more than several times in areas of the fault rupture. The stressed crust triggers resonance at frequencies varying from ~ 5 × 10–4 to ~ 10–3 Hz that is supported by the resonant frequency model.
Read more
Altmetrics
Final-revised paper
Preprint