Most of the minerals listed here - especially the native elements, the sulphides, the halides and the high-pressure minerals (e.g. coesite)- were found as microscopic inclusions in diamond. The others have been reported as constituents of the kimberlites.
Ref.:
- Wuyi Wang (1998): Formation of diamond with mineral inclusions of "mixed" eclogite and peridotite paragenesis. Earth and Planetary Science Letters 160(3/4), 831-843.
- Lu Fengxiang, Wang Ying, Chen Meihua, and Zheng Jianping (1999): Geochemical Characteristics and Emplacement Ages of the Mengyin Kimberlites, Shandong Province, China. In: Taylor, L.A., Snyder, G.A., Neal, C.R., and Ernst, W.G. (Eds.): Planetary Petrology and Geochemistry. Geological Society of America Publications, 277 pp.
- Gorshkov, A.I., Titkov, S.V., Yan Nan Bao, Ryabchikov, I.D., and Magazina, L.O. (2006): Microinclusions in Diamonds of Octahedral Habit from Kimberlites of Shandong Province, Eastern China. Geology of Ore Deposits 48(4), 326-334.
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Map Reference: 35°40'8"N , 117°46'40"E
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