“…4, Ba 2 Ce 3 (SiO 4 ) 3 F can be thought of as the evolution phase of the Ca 5 (PO 4 ) 3 F prototype obtained by co-substitution of [2Ba 2+ + 3Ce 3+ + 3SiO 4 4− ] for [5Ca 2+ + 3PO 4 3− ]. Based on the substitution of SiO 4 4− for PO 4 3− , a number of novel apatite-type compounds have been reported, including Ca 5 Y 3 Na 2 (PO 4 ) 5 (SiO 4 )F 2 , 88,89 Sr 9 La(PO 4 ) 5 (SiO 4 )F 2 , 90 Sr 4 La 6 (SiO 4 ) 6 F 2 , 91,92 NaLa 4 (SiO 4 ) 3 F, 93 SrMgY 3 (SiO 4 ) 3 F, 94 Ba 2 La 3 (SiO 4 ) 3 Cl, 95 Ca 9 La(PO 4 ) 5 (SiO 4 )Cl 2 , 96 and so on. 97–99 Similarly, GeO 4 4− can be adopted to replace PO 4 3− in materials to design a new apatite structural material Ba 2 La 3 (GeO 4 ) 3 F, reported by Ma et al , 100 and also SO 4 2− and BO 4 3− are used to acquire other apatite-type materials, such as K 3 Ca 2 (SO 4 ) 3 F, 101 Na 3 Ca 2 (SO 4 ) 3 F, 102 K 4 Sb(SO 4 ) 3 Cl, 103 Na 3 Pb 2 (SO 4 ) 3 Cl, 104 Na 3 Ca 2 (SO 4 ) 3 Cl 105 and Ca 5 (BO 4 ) 3 F. 106–108…”