摘要
The study of inclusions wrapped in diamonds concerns some important problemssuch as the formation of diamond and the characteristics and evolution of mantlelithosphere. Former workers divided solid diamond inclusions into two groups:theperidotitic type(P-type) and the eclogite type (E-type). Recently, MARID megacrystgroups, complex assemblage inclusions, salt, high potassic and chloric inclusionsare successively found in diamonds. Navon et al. (1988) and Menzies (1988)
基金
Project supported by the National Natural Science Foundation of China.
