scholarly journals Three-Dimensional Velocity Structure in Southwestern Japan and Configuration of the Philippine Sea Slab Estimated by Double-Difference Tomography

2007 ◽  
Vol 60 (1) ◽  
pp. 1-20 ◽  
Author(s):  
Fuyuki HIROSE ◽  
Junichi NAKAJIMA ◽  
Akira HASEGAWA
Keyword(s):  
Velocity Structure ◽  
Three Dimensional ◽  
Double Difference ◽  
Philippine Sea ◽  
Philippine Sea Slab

scholarly journals Three dimensional velocity structure around aftershock area of the 2004 mid Niigata prefecture earthquake (M6.8) by the Double-Difference tomography

2005 ◽  
Vol 57 (5) ◽  
pp. 429-433 ◽  
Author(s):  
Masahiro Korenaga ◽  
Satoshi Matsumoto ◽  
Yoshihisa Iio ◽  
Takeshi Matsushima ◽  
Kenji Uehira ◽  
...  
Keyword(s):  
Velocity Structure ◽  
Three Dimensional ◽  
Double Difference ◽  
Aftershock Area ◽  
Niigata Prefecture

scholarly journals Characteristics of relocated hypocenters of the 2018 M6.7 Hokkaido Eastern Iburi earthquake and its aftershocks with a three-dimensional seismic velocity structure

2019 ◽  
Vol 71 (1) ◽  
Author(s):  
Saeko Kita
Keyword(s):  
Seismic Velocity ◽  
Three Dimensional ◽  
Double Difference ◽  
Earthquake Catalog ◽  
Seismic Structure ◽  
Depth Limit ◽  
High Attenuation ◽  
South Central ◽  
Collision Zone ◽  
Hidaka Collision Zone

AbstractI relocated the hypocenters of the 2018 M6.7 Hokkaido Eastern Iburi earthquake and its surrounding area, using a three-dimensional seismic structure, the double-difference relocation method, and the JMA earthquake catalog. After relocation, the focal depth of the mainshock became 35.4 km. As previous studies show, in south-central Hokkaido, the Hidaka collision zone is formed, and anomalous deep and thickened forearc crust material is subducting at depths of less than 70 km. The mainshock and its aftershocks are located at depths of approximately 10 to 40 km within the lower crust of the anomalous deep and thickened curst near the uppermost mantle material intrusions in the northwestern edge of this Hidaka collision zone. Like the two previous large events, the aftershocks of this event incline steeply eastward and appear to be distributed in the deeper extension of the Ishikari-teichi-toen fault zone. The highly inclined fault in the present study is consistent with a fault model by a geodetic analysis with InSAR. The aftershocks at depths of 10 to 20 km are located at the western edge of the high-attenuation (low-Qp) zone. These kinds of relationships between hypocenters and materials are the same as the 1970 and 1982 events in the Hidaka collision zone. The anomalous large focal depths of these large events compared with the average depth limit of inland earthquakes in Japan could be caused by the locally lower temperature in south-central Hokkaido. This event is one of the approximately M7 large inland earthquakes that occurred repeatedly at a recurrence interval of approximately 40 years and is important in the collision process in the Hidaka collision zone.

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