The reactions of ringwoodite-octahedral diopside-octahedral tremolite were dealt with in this paper.
本文讨论了尖晶橄榄石的反应。
2
This change can be explained by different cation radiuses in the octahedral coordination site of garnet lattice.
这种规律性的变化可由石榴石晶格中处于八次配位时不同阳离子的配位半径不同作出解释。
3
Inner- and outer-sphere surface complexes of all such three cations with tetrahedral and octahedral charge sites were observed in the one-layer hydrates.