From: Source rupture process of the 2011 Fukushima-ken Hamadori earthquake: how did the two subparallel faults rupture?
Fault
Strike angle
Dip angle
Size
Latitude
Longitude
Depth
(°)
(km2)
(°N)a
(°E)a
(km)a
Itozawa fault
156
73
22 × 14
36.952
140.686
6.96
Yunodake fault
130
62
18 × 14
37.014
140.676
11.48