CAI Yitao, ZHANG Jie, KANG Congxuan, YANG Xianzhong, CAO Zhengqi, DONG Zhongdou, MA Yuguang, SHI Jianbin. 2019: Mineral chemistry characteristics of garnets in diamondiferous basite of Lan'gan area, Anhui Province. Geological Bulletin of China, 38(1): 110-120.
    Citation: CAI Yitao, ZHANG Jie, KANG Congxuan, YANG Xianzhong, CAO Zhengqi, DONG Zhongdou, MA Yuguang, SHI Jianbin. 2019: Mineral chemistry characteristics of garnets in diamondiferous basite of Lan'gan area, Anhui Province. Geological Bulletin of China, 38(1): 110-120.

    Mineral chemistry characteristics of garnets in diamondiferous basite of Lan'gan area, Anhui Province

    • The mafic rock is exposed in northern Anhui Province, and some of them are diamondiferous rocks. In order to determine the type of garnets, the authors systematically sampled the garnets in diamondiferous basite in Lan'gan area. The MgO, SiO 2, FeO, TiO2, Al2O3, Cr2O3, CaO, MnO values of 62 single crystal garnets in this area were measured by electron microprobe spectrometer. The results show that the chemical formula of garnet group minerals is A32+B23+(SiO4)3. Group A cations are composed of Mg2+, Fe2+ and Ca2+. Group B cations are composed of Al3+, Fe3+, Mn3+ and Cr3+. The trivalent cation is mainly Al3+ while divalent cation is mainly Ca2+. It is inferred that grossularite-andradite-almandine group is the primary class in the Lan'gan area. The high calcium silicate iron garnet (majorite) was found in 62 samples. According to the composition of these majorities in Lan'gan area, the garnet of the diamondiferous basite has formation pressure of 12.1~12.8GPa, and the depth is up to 300km.
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