h i g h l i g h t sWe have undertaken a study of huanghoite using vibrational spectroscopy. A comparison is made with spectra of other halogenated carbonates. Multiple carbonate stretching vibrations proved that there are non-equivalent carbonate units. Raman bands in the OH stretching region gives evidence for OH units in the huanghoite structure. a b s t r a c t Raman spectroscopy complimented with infrared spectroscopy has been used to study the rare earth based mineral huanghoite with possible formula given as BaCe(CO 3 ) 2 F and compared with the Raman spectra of a series of selected natural halogenated carbonates from different origins including bastnasite, parisite and northupite. The Raman spectrum of huanghoite displays three bands are at 1072, 1084 and 1091 cm À1 attributed to the CO 2À 3 symmetric stretching vibration. The observation of three symmetric stretching vibrations is very unusual. The position of CO 2À 3 symmetric stretching vibration varies with mineral composition. Infrared spectroscopy of huanghoite show bands at 1319, 1382, 1422 and 1470 cm À1 . No Raman bands of huanghoite were observed in these positions. Raman spectra of bastnasite, parisite and northupite show a single band at 1433, 1420 and 1554 cm À1 assigned to the m 3 (CO 3 ) 2À antisymmetric stretching mode. The observation of additional Raman bands for the m 3 modes for some halogenated carbonates is significant in that it shows distortion of the carbonate anion in the mineral structure. Four Raman bands for huanghoite are observed at 687, 704, 718 and 730 cm À1 and assigned to the (CO 3 ) 2À m 2 bending modes. Raman bands are observed for huanghoite at around 627 cm À1 and are assigned to the (CO 3 ) 2À m 4 bending modes. Raman bands are observed for the carbonate m 4 in phase bending modes at 722 cm À1 for bastnasite, 736 and 684 cm À1 for parisite, 714 cm À1 for northupite. Raman bands for huanghoite observed at 3259, 3484 and 3589 cm À1 are attributed to water stretching bands. Multiple bands are observed in the OH stretching region for bastnasite and parisite indicating the presence of water and OH units in their mineral structure. Vibrational spectroscopy enables new information on the structure of huanghoite to be assessed.