Results (
Thai) 3:
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sidered as potential lower-mantle phase constituents.
In addition to the diamond-bearing phases, megacrysts of baddeleyite
from the Mbuji Mayi kimberlites have been suggested as having
originated in the lower-mantle, presumably having transformed from
a cubic ZrO2 lower mantle structure to their present upper mantle
monoclinic lattice
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