Infrared and Raman spectra have been used extensively for the characterisat
ion of the mineral component of mineralised tissues, especially bone and te
eth. Often the vibrational modes of hydroxy groups and hydrogen phosphate a
re masked in the presence of substituent anions such as carbonate. The inel
astic neutron scattering (INS) spectra are dominated by the vibrations of g
roups with hydrogen or with hydrogen riding on groups. Two sets of bands ha
ve been assigned to the hydroxy librations related to the hexagonal and mon
oclinic polymorphs of hydroxyapatite. Of the phosphate bands in brushite on
ly the HPO42- bands are seen in the INS spectrum. These INS studies of synt
hetic hydroxyapatites and brushite present new opportunities for studying a
spects of biominerals not accessible by standard vibrational techniques.