摘要
Recently mineral inclusions and diamonds containing these inclusions are divided into three suites: the peridotite, the eclogite and the late crystallizing megacryst suites by ways of the mineralogical and chemical composition, and the isotopic characteristic of inclusions of diamonds. Since the 1960s some odd investigations about the mineral inclusions of diamonds were carried out in China. This is the first re-
基金
Project supported by the National Natural Science Foundation of China.
