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Fate of MgSiO(3) melts at core–mantle boundary conditions
One key for understanding the stratification in the deep mantle lies in the determination of the density and structure of matter at high pressures, as well as the density contrast between solid and liquid silicate phases. Indeed, the density contrast is the main control on the entrainment or settlem...
Wedi'i Gadw mewn:
| Cyhoeddwyd yn: | Proc Natl Acad Sci U S A |
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| Prif Awduron: | , , , , , , , , |
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
National Academy of Sciences
2015
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| Pynciau: | |
| Mynediad Ar-lein: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4655538/ https://ncbi.nlm.nih.gov/pubmed/26578761 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1512386112 |
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