Based on previous studies of kimberlite xenoliths and diamond inclusions in this region, macrocrystai garnet was analyzed with the electric microprobe technique （EPMA）. The garnet is collected from the Shengli No.1 ...Based on previous studies of kimberlite xenoliths and diamond inclusions in this region, macrocrystai garnet was analyzed with the electric microprobe technique （EPMA）. The garnet is collected from the Shengli No.1 kimberlite pipe in the Mengyin area of Shandong Province, China. The results indicate that the garnet contains two kinds of multiphase inclusions： one is K-, B-, and CI- bearing oxygen-free phase, K- and Cl-bearing oxygen-free phase, and volatile-bearing garnet inclusions （in1 and in3）; and the other is chlorite, phlogopite, apatite and calcite （in2）. It is suggested that the formation of garnet and its inclusions is associated with strongly reduced mantle fluid. Such a fluid was transformed from ultra-deep high-reduction oxygen-free fluid into low-reduction alkaline fluid, and finally into oxidized fluid with low oxygen fugacity. This result confirms that the Mengyin area underwent metamorphism of slightly active deep fluid, and provides evidence for searching diamond by means of indicative minerals.展开更多
基金supported by the National Natural Science Foundation of China (Grant No. 4027301)the National Geological Survey Project (Grant No.003201)
文摘Based on previous studies of kimberlite xenoliths and diamond inclusions in this region, macrocrystai garnet was analyzed with the electric microprobe technique （EPMA）. The garnet is collected from the Shengli No.1 kimberlite pipe in the Mengyin area of Shandong Province, China. The results indicate that the garnet contains two kinds of multiphase inclusions： one is K-, B-, and CI- bearing oxygen-free phase, K- and Cl-bearing oxygen-free phase, and volatile-bearing garnet inclusions （in1 and in3）; and the other is chlorite, phlogopite, apatite and calcite （in2）. It is suggested that the formation of garnet and its inclusions is associated with strongly reduced mantle fluid. Such a fluid was transformed from ultra-deep high-reduction oxygen-free fluid into low-reduction alkaline fluid, and finally into oxidized fluid with low oxygen fugacity. This result confirms that the Mengyin area underwent metamorphism of slightly active deep fluid, and provides evidence for searching diamond by means of indicative minerals.
