Search for deep slabs in the Northwest Pacific mantle
A residual sphere is formed by projecting seismic ray travel-time anomalies, relative to a reference Earth model, onto an imaginary sphere around an earthquake. Any dominant slab-like fast band can be determined with spherical harmonic expansion. The technique is useful in detecting trends associate...
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| Publicat a: | Proc Natl Acad Sci U S A |
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| Autors principals: | , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
1989
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC298334/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/16594080/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.86.22.8602 |
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