Citation: Brovkin, A. A.; Rozhdestvenskaya, I. V.; Rykova, E. A. (2002). Cation distribution in the structure of titanium-containing ludwigite Note: to be the mineral azoproite, Ti+Mg must be greater than Fe3+ in M4 site Note: Uiso values have been divided by 100. Crystallography Reports, 47, pp. 412-414.