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• W2007219314 endingPage "1074" @default.
• W2007219314 startingPage "1071" @default.
• W2007219314 abstract "Densities of molten silicates at high pressures (up to approximately 230 kilobars) have been measured for the first time with shock-wave techniques. For a model basaltic composition (36 mole percent anorthite and 64 mole percent diopside), a bulk modulus K(s), of approximately 230 kilobars and a pressure derivative (dK(s)/dP) of approximately 4 were derived. Some implications of these results are as follows: (i) basic to ultrabasic melts become denser than olivine-and pyroxene-rich host mantle at pressures of 60 to 100 kilobars; (ii) there is a maximum depth from which basaltic melt can rise within terrestrial planetary interiors; (iii) the slopes of silicate solidi [(dT(m)/dP), where T(m) is the temperature] may become less steep at high pressures; and (iv) enriched mantle reservoirs may have developed by downward segregation of melt early in Earth history." @default.
• W2007219314 created "2016-06-24" @default.
• W2007219314 creator A5018925530 @default.
• W2007219314 creator A5039613093 @default.
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• W2007219314 date "1984-11-30" @default.
• W2007219314 modified "2023-09-26" @default.
• W2007219314 title "Densities of Liquid Silicates at High Pressures" @default.
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• W2007219314 doi "https://doi.org/10.1126/science.226.4678.1071" @default.
• W2007219314 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/17839996" @default.
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