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- W2601025511 abstract "Recent shock data for TiO_2 and SiO_2, when taken with static results for RuO_2 and HfO_2suggest that this group of oxides transforms from the 6-fold coordinated rutile structure to the 8-foldcoordinated fluorite structure which is 7-8 % denser than rutile. In the case of SiO_2, the transitionto a fluorite structure may be representative of the lower mantle silicate transitions which couldoccur in the D zone. There may be technological interest in the fluorite-structured oxides becausethese are predicted to be as hard or harder than cubic boron nitride. In the case of fluorite-structuredSiO_2 and HfO_2 hardnesses, comparable or greater than diamond are predicted." @default.
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- W2601025511 date "1996-01-01" @default.
- W2601025511 modified "2023-09-27" @default.
- W2601025511 title "Geophysical and Material Science Implications of the Post-Stishovite Phase" @default.
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