April 10, 2018
Earthquake Research Committee,
Headquarters for Earthquake Research Promotion
On March 1, there was a magnitude (M) 5.6 earthquake near Iriomotejima. Maximum seismic intensity 5 Lower was observed in Okinawa prefecture.
There was no remarkable activity.
* On March 23, there was an M5.1 earthquake at a depth of approximately 45 km, offshore Miyagi prefecture. The focal mechanism showed a reverse fault type with a compression axis in a WNW-ESE direction. This event occurred at the boundary between the Pacific and the continental plates.
* On March 13, there was an M4.9 earthquake at a depth of approximately 50 km under the northeastern Chiba prefecture. The focal mechanism had a compression axis in a WNW-ESE direction.
* On March 25, there was an M5.8 earthquake offshore east of Hachijojima. The focal mechanism showed a reverse fault type with a compression axis in a WNW-ESE direction. This event occurred within the Pacific plate.
* On March 30, there was an M5.1 earthquake at a depth of approximately 55 km, offshore Ibaraki prefecture [under the northern Ibaraki prefecture]. The focal mechanism showed a reverse fault type with a compression axis in a WNW-ESE direction. This event occurred at the boundary between the Pacific and the continental plates.
There was no remarkable activity.
* 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.
* 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.
* On April 9 at 01:32 (JST), there was an M6.1 earthquake at a depth of approximately 10 km in the western Shimane prefecture. Maximum seismic intensity 5 Upper was observed in Shimane prefecture. This event occurred within the crust. The focal mechanism showed a strike-slip fault type with a compression axis in an NNW-SSE direction (preliminary). The seismic fault is estimated to be a left-lateral strike-slip one extending in an NNW-SSE direction. In the vicinity of this event, there were 4 earthquakes with maximum seismic intensity 4 until April 10 at 15 o'clock, including an M4.8 (preliminary) earthquake which occurred on April 9 at about 02:10 (JST).
Note: [ ] is the regional name of the epicenter used in the Japan Meteorological Agency announcement.
April 10, 2018
Earthquake Research Committee
The following are the numbers of earthquakes by magnitude (M) that occurred in Japan and the surrounding area during March 2018.
(reference)
The following events for the period from March 2017 to late February 2018 have been listed as "Major Seismic Activities" in monthly "Evaluation of Seismic Activities."
– 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) |
There is no supplementary information for Hokkaido region.
There is no supplementary information for Tohoku region.
There is no supplementary information for Kanto-Chubu region.
– Near the boundary between the Philippine Sea and the continental plates, from Tokushima prefecture to the Bungo Channel, deep low-frequency earthquakes (tremors) were observed in the period from February 21 to March 31. Also due to the strain-inclination data, slight crustal deformation was observed in Ehime and Kochi prefectures and its surroundings from late February to late March. Also GNSS data showed a slight crustal deformation from late February. These phenomena are considered to be caused by the short-term slow-slip at the boundary between the Philippine Sea and the continental plates.
–";On March 1, there was an M5.6 earthquake at a depth of approximately 15 km near Iriomotejima. (Exerpted)":
After this event, the seismic activity became high and there were 40 earthquakes with maximum seismic intensity 1 or over until March 31.
–"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 April 6 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, April 6, 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)"
Reference 1
Earthquakes that are described in the "Evaluation of Seismic Activity"
(Monthly Report of Seismic Activity in Japan) have the following
features.
Reference 2
Information that is described in the "Supplementary Information to the Evaluation" includes: