地球科学

• 钙铝榴石

  Blocks of garnet-pyroxenite or rodingite are locally present in the meta-peridotite. Garnets in the cumulates are grossular (Gro 69.19-89.93;And 9.12-18.84;Br 0.73-11.63), formed by metamorphism.

  石榴石辉石岩或异剥钙榴岩呈团块状产于变质橄榄岩中,其中的石榴石为钙铝榴石(Gro69.19%～89.93%;And9.12%～18.84%;Br0.73%～11.63%),也属变质成因。

• 钙铝榴石宝石

• 钙铝石榴子石