18 results on '"Kaneda, Yoshiyuki"'
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2. S wave attenuation structure on the western side of the Nankai subduction zone: Implications for fluid distribution and dynamics.
3. Seismic constraints of the formation process on the back-arc basin in the southeastern Japan Sea.
4. Evolution from fore-arc oceanic crust to island arc crust: A seismic study along the Izu-Bonin fore arc.
5. Detailed structural image around splay-fault branching in the Nankai subduction seismogenic zone: Results from a high-density ocean bottom seismic survey.
6. Structure and growth of the Izu-Bonin-Mariana arc crust: 1. Seismic constraint on crust and mantle structure of the Mariana arc-back-arc system.
7. Seismological evidence for variable growth of crust along the Izu intraoceanic arc.
8. A cause of rupture segmentation and synchronization in the Nankai trough revealed by seismic imaging and numerical simulation.
9. Seismicity in the incoming/subducting Philippine Sea plate off the Kii Peninsula, central Nankai trough.
10. Variation of physical properties beneath a fault observed by a two-ship seismic survey off southwest Japan.
11. Structural factors controlling the coseismic rupture zone of the 1973 Nemuro-Oki earthquake, the southern Kuril Trench seismogenic zone.
12. Microseismicity at the seaward updip limit of the western Nankai Trough seismogenic zone.
13. Seismic structure of western end of the Nankai trough seismogenic zone.
14. A deep strong reflector in the Nankai accretionary wedge from multichannel seismic data: Implications for underplating and interseismic shear stress release.
15. Crustal structure across the coseismic rupture zone of the 1944 Tonankai earthquake, the central Nankai Trough seismogenic zone.
16. Tectonic features of the Japan Trench convergent margin off Sanriku, northeastern Japan, revealed by multichannel seismic reflection data.
17. Correction to 'Crustal structure across the coseismic rupture zone of the 1944 Tonankai earthquake, the central Nankai Trough seismogenic zone'.
18. Correction to 'A cause of rupture segmentation and synchronization in the Nankai trough revealed by seismic imaging and numerical simulation'.
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