Bending-Related Topographic Structures of the Subducting Plate in the Northwestern Pacific Ocean - Accretionary Prisms and Convergent Margin Tectonics in the Northwest Pacific Basin - page 20

144°E 145°E

41°N 41°N

ER

40°N 40°N

39°N 39°N

38°N 38°N

144°E 145°E

Fig. 12 Distribution of bending-related topographic structures in the northern Japan Trench.
Conventions are identical to Fig. 9

3.3.3 Izu-Ogasawara Trench

The Izu-Ogasawara Trench physiographically terminates at the subducting
Daiichi-Kashima Seamount. The northernmost portion of the Izu-Ogasawara Trench
forms the trench-trench-trench triple junction with Sagami Trough. The seafloor of