Single crystals of carbonate apatite were grown using a CaCO3 flux under an
Ar gas pressure of 55 MPa. The crystals obtained were observed by scanning
electron microscopy, optical microscopy and X-ray diffraction. Electron pr
obe microanalyses and thermal analyses were performed. CO3 ions in planar t
riangle form replaced both OH sites and PO4 tetrahedral sites in the apatit
e structure: in particular, the OH sites were perfectly substituted by CO3
ions using this method. (C) 1999 Kluwer Academic Publishers.