Additional file 11 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands

Supplementary file 11. Figure S11 Velocity difference of S 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

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Publication Details

Journal
Figshare
Published
2025-01-01
DOI
https://doi.org/10.6084/m9.figshare.29595421
Primary Topic
Seismic Imaging and Inversion Techniques
Type
article
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Additional file 11 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands

Figshare
Seismic Imaging and Inversion Techniques
article

Additional file 11 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands

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Abstract

Supplementary file 11. Figure S11 Velocity difference of S 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

Figshare
Japan Meteorological Agency (JP), University of Toyama (JP)
Life below water
Openalex Percentile: Top 51%
Seismic Imaging and Inversion Techniques
DOIOpen Access PDFOpenAlex
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Additional file 11 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands · Figshare (2025) | TGRS Research Map | TGRS