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Topology of the postperovskite phase transition and mantle dynamics
The postperovskite (ppv) phase transition occurs in the deep mantle close to the core–mantle boundary (CMB). For this reason, we must include in the dynamical considerations both the Clapeyron slope and the temperature intercept, T(int), which is the temperature of the phase transition at the CMB pr...
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| Päätekijät: | , |
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| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
National Academy of Sciences
2007
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| Aiheet: | |
| Linkit: | https://ncbi.nlm.nih.gov/pmc/articles/PMC1890463/ https://ncbi.nlm.nih.gov/pubmed/17483485 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0608480104 |
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