| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4693018 | Tectonophysics | 2011 | 9 Pages |
Abstract
⺠The aftershocks of the 2010 Ryukyu earthquake trend toward the ENE-WSW direction. ⺠Double seismic structure exists in the Philippine Sea plate of the central Ryukyu. ⺠The earthquakes with compression stress occur in the crust of the subducted plate. ⺠The aftershocks with extension stress occur in the mantle of the subducted plate.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Mamoru Nakamura,