April 11, 2017
Earthquake Research Committee,
Headquarters for Earthquake Research Promotion
There was no remarkable activity.
* On March 14, there was a magnitude (M) 4.7 earthquake at a depth of approximately 80 km under the western Hidaka region. The focal mechanism had a tension axis in an NE-SW direction. This event occurred within the Pacific plate.
* On March 8, there was a M5.2 earthquake at a depth of approximately 65 km, offshore east of Aomori 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 12, there was a M5.4 earthquake at a depth of approximately 45 km, offshore Fukushima 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 5, there was a M4.7 earthquake at a depth of approximately 50 km under the northeastern Chiba prefecture. The focal mechanism showed a reverse fault type with a compression axis in an E-W direction. This event occurred at the boundary between the Pacific and the Philippine Sea plates.
* In the GNSS data for the Tokai region, there has been no change of activity which is likely to be associated with the Tokai earthquake.
There was no remarkable activity.
* On March 2, there was a M5.3 earthquake at a depth of approximately 35 km under Hyuganada. The focal mechanism showed a normal fault type with a tension axis in an E-W direction. This event occurred within the Philippine Sea plate.
* On March 12, there was a M5.1 earthquake at a depth of approximately 140 km under the ocean area near Tanegashima [Offshore west of Satsuma Peninsula]. The focal mechanism had a tension axis in the subducting direction of the Philippine Sea plate. This event occurred within the Philippine Sea plate.
* On March 25, there was a M5.1 earthquake at a depth of approximately 85 km under the ocean area near Okinawa main island. The focal mechanism had a compression axis in an NNW-SSE direction. This event occurred within the Philippine Sea plate.
Note: [ ] is the regional name of the epicenter used in the Japan Meteorological Agency announcement.
GNSS (Global Navigation Satellite System) is a general name of satellite
positioning system such as GPS.
April 11, 2017
Earthquake Research Committee
The following are the numbers of earthquakes by magnitude (M) that occurred in Japan and the surrounding area during March 2017.
(reference)
The following events for the period from March 2016 to late February 2017 have been listed as "Major Seismic Activities" in monthly "Evaluation of Seismic Activities."
– Kumamoto Earthquakes | M6.5 on April 14, 2016 and M7.3 on April 16, 2016 (Depth of approximately 10 km) |
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– Southern Ibaraki Prefecture | M5.5 on May 16, 2016 (Depth of approximately 40 km) |
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– Uchiura Bay | M5.3 on June 16, 2016 (Depth of approximately 10 km) |
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– Northern Ibaraki Prefecture | M5.4 on July 27, 2016 (Depth of approximately 55 km) |
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– Kumamoto Region, Kumamoto Prefecture | M5.2 on August 31, 2016 (Depth of approximately 15 km) |
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– Ocean Area near Okinawa Main Island | M5.6 on September 26 (Depth of approximately 45 km) |
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– Central Tottori Prefecture | M6.6 on October 21, 2016 (Depth of approximately 10 km) |
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– Offshore Fukushima Prefecture | M7.4 on November 22, 2016 (Depth of approximately 10 km) |
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– Northern Ibaraki Prefecture | M6.3 on December 28, 2016 (Depth of approximately 10 km) |
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– Offshore Fukushima Prefecture | M5.7 on February 28, 2017 (Depth of approximately 50 km) |
There is no supplementary information for Hokkaido region.
There is no supplementary information for Tohoku region.
–"In the GNSS data for the Tokai region, there has been no change
of activity which is likely to be associated with the Tokai earthquake.":
(This evaluation is in agreement with the views presented at the regular
meeting on March 27 of the Assessment Committee for Areas under Intensified
Measures against Earthquake Disaster (reference below).)
(Reference)
Recent seismic and crustal activity in the Tokai region and its vicinity (Seismological and Volcanological Department, Japan Meteorological Agency, March 27, 2017)
"No change of activity which is likely to be associated with the Tokai earthquake has been observed until now. (Excerpted)"
There is no supplementary information for Kinki-Chugoku-Shikoku region.
– In March, no earthquake with maximum seismic intensity 4 or over
(0 in February) and 1 earthquake with maximum seismic intensity 3 (1 in
February) occurred in the Kumamoto and Aso regions, Kumamoto prefecture.
A series of seismic activity of the 2016 Kumamoto Earthquakes in the Kumamoto
and Aso regions still continues, decaying as a whole, and the seismic activity
of present will continue for a while. According to the GNSS observation,
postseismic deformation in the area centered on the series of the seismic
activity is converging as a whole.
A year has passed since the occurrence of the 2016 Kumamoto earthquakes. Note that in Kyushu region, there are several examples of an occurrence of an earthquake of the same order magnitude in a few years after an earthquake of M6.0 or so, such as the 1889 Kumamoto earthquake.
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: