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Shear waves in the diamond-anvil cell reveal pressure-induced instability in (Mg,Fe)O
The emerging picture of Earth's deep interior from seismic tomography indicates more complexity than previously thought. The presence of lateral anisotropy and heterogeneity in Earth's mantle highlights the need for fully anisotropic elasticity data from mineral physics. A breakthrough in...
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| Autors principals: | , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2004
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC395889/ https://ncbi.nlm.nih.gov/pubmed/15079080 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0401564101 |
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