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...

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Detaylı Bibliyografya
Yayımlandı:Proc Natl Acad Sci U S A
Asıl Yazarlar: Petitgirard, Sylvain, Malfait, Wim J., Sinmyo, Ryosuke, Kupenko, Ilya, Hennet, Louis, Harries, Dennis, Dane, Thomas, Burghammer, Manfred, Rubie, Dave C.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: National Academy of Sciences 2015
Konular:
Physical Sciences
Online Erişim: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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