June 9, 2017
Earthquake Research Committee,
Headquarters for Earthquake Research Promotion
There was no remarkable activity.
* On May 22, there was a magnitude (M) 5.7 earthquake at a depth of approximately 60 km (CMT solution) offshore east of Hokkaido. The focal mechanism showed a reverse fault type with a compression axis in a WNW-ESE direction. This event occurred within the Pacific plate.
There was no remarkable activity.
* 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 May 4, there was an M4.1 earthquake at a depth of approximately 10 km in the Kumamoto region, Kumamoto prefecture. The focal mechanism showed a normal fault type with a tension axis in an NNW-SSE direction. This event occurred within the crust.
* On May 9, there was an M6.4 earthquake at a depth of approximately 20 km (CMT solution) under the ocean area near Miyakojima. The focal mechanism showed a strike-slip fault type with a tension axis in an NNW-SSE direction.
* On May 11, there was an M4.4 earthquake at a depth of approximately 15 km in the Ariake Sea [Kumamoto region, Kumamoto prefecture]. The focal mechanism showed a normal fault type with a tension axis in an N-S direction. This event occurred within the crust.
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.
June 9, 2017
Earthquake Research Committee
The following are the numbers of earthquakes by magnitude (M) that occurred in Japan and the surrounding area during May 2017.
(reference)
The following events for the period from May 2016 to late April 2017 have been listed as "Major Seismic Activities" in monthly "Evaluation of Seismic Activities."
– 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 May 29 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, May 29, 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.
–"On May 4, there was an M4.1 earthquake at a depth of approximately
10 km in the Kumamoto region, Kumamoto prefecture. (Excerpted) " "On
May 11, there was an M4.4 earthquake at a depth of approximately 15 km
in the Ariake Sea [Kumamoto region, Kumamoto prefecture]. (Excerpted) ":
In May, 2 earthquakes (0 in April) with maximum seismic intensity 4 or
over and 1 earthquake (1 in April) with maximum seismic intensity 3 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 at 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.
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: