Additional file 6 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands

Supplementary file 6. Figure S6 Velocity difference of P wave from the initial model for restoring constraint $$w^{2}_{r}$$ w r 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.29595406
Primary Topic
Seismic Imaging and Inversion Techniques
Type
article
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article

Additional file 6 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands

Figshare
Seismic Imaging and Inversion Techniques
article

Additional file 6 of Three-dimensional velocity structure model for hypocenter determination in and around the Japanese Islands

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Abstract

Supplementary file 6. Figure S6 Velocity difference of P wave from the initial model for restoring constraint $$w^{2}_{r}$$ w r 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 55%
Seismic Imaging and Inversion Techniques
DOIOpen Access PDFOpenAlex
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