Su, Ben-Xun; Zhang, Hongfu; Sakyi, Patrick Asamoah; Qin, Ke-Zhang; Liu, Pingping; Ying, Jifeng; Tang, Yanjie; Malaviarachchi, Sanjeewa; Yan, Xiao; Zhao, Xinmaio; Mao, Qian; Ma, Yuguang
Two types of melt pockets, closed melt pocket (CMP) and open melt pocket (OMP), are recognized from the peridotite xenoliths entrained in the Cenozoic kamafugites in western Qinling (Chinese Source), Central China. The Haoti (Chinese Source) CMPs have a mineral assemblage of olivine+ clinopyroxene+amphibole+K-feldspar, whereas the Baiguan (Chinese Source) CMPs are composed of olivine+clinopyroxene+ilmenite+carbonate. The components of the OMPs are more complicated. In the Haoti OMPs, there are...[Show more]
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