March 9, 2018
Earthquake Research Committee,
Headquarters for Earthquake Research Promotion

Evaluation of Seismic Activities for February 2018

1 Major Seismic Activities

There was no remarkable activity.

2 Nationwide Seismic Activities by Region

(1) Hokkaido Region

There was no remarkable activity.

(2) Tohoku Region

* On February 26, there was a magnitude (M) 5.8 earthquake at a depth of approximately 40 km, offshore Fukushima prefecture. The focal mechanism showed a reverse fault type with a compression axis in an NNW-SSE direction.

(3) Kanto-Chubu Region

* On February 13, there was an M4.1 earthquake at a depth of approximately 5 km in the southern Nagano prefecture. The focal mechanism had a compression axis in a WNW-ESE direction. This event occurred within the crust.

(4) Kinki-Chugoku-Shikoku Region

* On February 19, there was an M5.0 earthquake at a depth of approximately 40 km under the Bungo Channel. The focal mechanism showed a normal fault type with a compression axis in an NW-SE direction. In addition there was another M5.0 earthquake at almost the same time and the place. Both earthquakes occurred within the Philippine Sea plate.

(5) Kyushu-Okinawa Region

There was no remarkable activity.

(6) Around the Nankai Trough

* There has been observed no unusual change which indicates that the possibility of occurrence of great earthquakes along the Nankai Trough has relatively raised compared to the normal time.

(7) Other Regions

* On February 7 (JST time), there was an M6.7 earthquake at a depth of approximately 10 km near Taiwan. The focal mechanism had a compression axis in an N-S direction. In the vicinity of the recent event, the seismic activity has become high from February 4; On February 4, there was an M6.5 earthquake and there were 4 earthquakes of M6.0 or over until February 28. In addition, according to the results from Synthetic Aperture Radar Interferometry Analysis of data by the Advanced Land Observing Satellite-2 "DAICHI-2", a discontinuity in the surface displacement is found in the eastern Taiwan and the crustal deformation of the enormous rise is observed in its eastern side.

Supplement

* On March 1, there was an M5.6 earthquake at a depth of approximately 15 km near Iriomotejima. The focal mechanism had a tension axis in an NE-SW direction. This event occurred within the continental crust.



Supplementary Information to the Evaluation of Seismic Activities for February 2018

March 9, 2018
Earthquake Research Committee

1 Major Seismic Activities

The following are the numbers of earthquakes by magnitude (M) that occurred in Japan and the surrounding area during February 2018.

(reference)

The following events for the period from February 2017 to late January 2018 have been listed as "Major Seismic Activities" in monthly "Evaluation of Seismic Activities."

  – Offshore Fukushima Prefecture  M5.7 on February 28, 2017
(Depth of approximately 50 km)
  – Bungo Channel  M5.0 on June 20, 2017
(Depth of approximately 40 km)
  – Southern Nagano Prefecture  M5.6 on June 25, 2017
(Depth of approximately 5 km)
  – Central and Eastern Iburi Region  M5.1 on July 1, 2017
(Depth of approximately 25 km)
  – Aso Region, Kumamoto Prefecture  M4.5 on July 2, 2017
(Depth of approximately 10 km)
  – Kagoshima Bay  M5.3 on July 11, 2017
(Depth of approximately 10 km)
  – Southern Inland, Akita Prefecture  M5.2 on September 8, 2017
(Depth of approximately 10 km)
  – Offshore Fukushima Prefecture  M5.9 on October 6, 2017
(Depth of approximately 55 km)

2 Nationwide Seismic Activities by Region

(1) Hokkaido Region

There is no supplementary information for Hokkaido region.

(2) Tohoku Region

There is no supplementary information for Tohoku region.

(3) Kanto-Chubu Region

There is no supplementary information for Kanto-Chubu region.

(4) Kinki-Chugoku-Shikoku Region

– Near the boundary between the Philippine Sea and the continental plates, from Ehime prefecture to the Bungo Channel, deep low-frequency earthquakes (tremors) are observed from February 21. Also due to the strain-inclination data, slight crustal deformation is observed in Ehime and Kochi prefectures from February 21. These phenomena are considered to be caused by the slow-slip in the short interval at the boundary between the Philippine Sea and the continental plates.

(5) Kyushu-Okinawa Region

There is no supplementary information for Kyushu-Okinawa region.

(6) Around the Nankai Trough

–"There has been observed no unusual change which indicates that the possibility of occurrence of great earthquakes along the Nankai Trough has relatively raised compared to the normal time.":
(This evaluation is in agreement with the views presented at the regular meeting on February 26 of the Assessment Committee for Earthquakes along the Nankai Trough (reference below).)

(Reference)

Recent crustal activity around the Nankai Trough (Seismological and Volcanological Department, Japan Meteorological Agency, February 29, 2018)
"In the present, there has been observed no unusual change which indicates that the possibility of occurrence of great earthquakes along the Nankai Trough has relatively raised compared to the normal time.(Excerpted)"

(7) Other Regions

There is no supplementary information for other regions.

Reference 1
Earthquakes that are described in the "Evaluation of Seismic Activity" (Monthly Report of Seismic Activity in Japan) have the following features.

  1. Events of M6.0 or greater, or events that have maximum seismic intensity 4 or greater
  2. Onshore events of M4.5 or greater that have maximum seismic intensity 3 or greater
  3. Events under the ocean areas of M5.0 or greater that have maximum seismic intensity 3 or greater

Reference 2
Information that is described in the "Supplementary Information to the Evaluation" includes:

  1. Reference information related to the seismic activity described in the "Evaluation of Seismic Activity"
  2. Recent earthquake activity over the past year related to the events described in "Major Seismic Activity" in the "Evaluation of Seismic Activity"
  3. Seismic activity that has been evaluated, but not included in the "Evaluation of Seismic Activity" because it is within normal bounds and not prominent
  4. A sequence of slow-slip events of estimated M6.0 or greater and accompanying low-frequency earthquakes (tremors)