Report of activity
Abstract of the 211th meeting of CCEP
The 211th meeting of the Coordinating Committee for Earthquake Prediction(CCEP) was held at the Kanto Regional Survey Department of the GSI on May 18, 2016.
First of all, nationwide monitoring data of the seismic activity and the crustal deformation were reported. After that, we discussed 2016 Kumamoto earthquakes.
Please see to the overviews below.
Documents (PDF:55MB)
- Deliberation about crusutal activity monitoring.
- 2016 Kumamoto earthquakes p.19 (Hirata (Professor), ERI)
1.1 General crusutal activities.
(1)Seismic activities of Japan.
p.3 (JMA)
(2)Activity of shallow very-low-frequency earthquakes around Japan.
p.4 (NIED)
(3)Strain changes in the Japanese Islands.
p.5 (GSI)
1.2 The 2011 off the Pacific coast of Tohoku Earthquake.
pp.6-7 (GSI)
p.8 (JCG)
1.3 The coupling state and change on the plate boundary.
(1)Suruga-trough, Nankai-trough and around the Nansei-shoto trench.
Unsteady crustal deformation in Kii channel pp.9-10(GSI)
Unsteady crustal deformation arround Bungo channel pp.11-12(GSI)
Activity of shallow very-low-frequency earthquakes and short-term SSE in southwest Japan p.13 (NIED)
Earthquake in southeast Mie Pref. p.14 (JMA) p.15 (NIED) pp.16 (JMA)
(1) Background
Outline of the earthquakes pp.20-22 (JMA)
Stress fields p.23 (Kyushu University))
(2) Monitoring
Distribution of seismic intensity pp.24-25 (JMA)
Stress field, sorce process, dristribution of hypocenter, crustal deformation pp.26-30 (NIED) pp.31-34 (Kyushu University))
Crustal deformation pp.35-37 (GSI)
Investigation of surface faulting pp.38-43 (AIST) p.44 (Kumahara (Associate Professor), Hiroshima University))
(3)Discussion about futuristic activity
Stochastic prediction of foreshock and aftershock activity p.45 (ISM)
Postseismic pp. 46-47 (GSI)
The relationship between Hyuga-nada and Kyushu inland earthquake pp.48-49 (Nagoya University))
Changes of static stress due to Kumamoto earthquake p.50 (Tohoku University))
- Purport of next intensive discussion subject "Postseismic slip and viscoelasticity".