Thermodynamic data for platinum group (Os, Ir, Ru, Rh, Pd and Pt) minerals are very limited. The present study is focused on the calculation of the Gibbs free energy of formation (∆ f G˝) for selected PGM occurring in layered intrusions and ophiolite complexes worldwide, applying available experimental data on their constituent elements at their standard state (∆G = G (species)´∆ G (elements) ), using the computer program HSC Chemistry software 6.0. The evaluation of the accuracy of the calculation method was made by the calculation of (∆G f ) of rhodium sulfide phases. The calculated values were found to be in good agreement with those measured in the binary system (Rh + S) as a function of temperature by previous authors (Jacob and Gupta (2014). The calculated Gibbs free energy (∆ f G˝) followed the order RuS 2 < (Ir,Os)S 2 < (Pt, Pd)S < (Pd, Pt)Te 2 , increasing from compatible to incompatible noble metals and from sulfides to tellurides.