Additional file 10 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands
Supplementary file 10. Figure S10 Velocity difference of P wave from the initial model for smoothing constraint $$w^{2}_{g}$$ w g 2 = 10, 0, 100. In (a)–(d), cross-sections of various latitudes are shown. The broken curve shows the slab top depth
Institutions
- Japan Meteorological Agency (JP)
- University of Toyama (JP)
Publication Details
- Journal
- Figshare
- Published
- 2025-01-01
- DOI
- https://doi.org/10.6084/m9.figshare.29595418.v1
- Primary Topic
- Wheat and Barley Genetics and Pathology
- Type
- article
- Field-Weighted Citation Impact
- 0.00