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Deep mantle structure as a reference frame for movements in and on the Earth
Earth’s residual geoid is dominated by a degree-2 mode, with elevated regions above large low shear-wave velocity provinces on the core–mantle boundary beneath Africa and the Pacific. The edges of these deep mantle bodies, when projected radially to the Earth’s surface, correlate with the reconstruc...
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| Main Authors: | , , , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
National Academy of Sciences
2014
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| Assuntos: | |
| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4066531/ https://ncbi.nlm.nih.gov/pubmed/24889632 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1318135111 |
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