During coking processes, certain coal-associated minerals undergo various chemical changes, amongst which are dehydration, dehydroxylation, and decarbonation. In order to evaluate the character of CO 2 and H 2 O emission by a particular mineral, thermodynamic calculations for theoretical gas production were performed. Observations showed that the behavior of carbonates in respect of CO 2 emission vary substantially and, for that reason, their influence on the properties of coke differ. The amount of mineral-associated CO 2 released during the coking process is smaller than that which is produced by a carbonbased matrix. For each ton of coal, containing 1 wt% of carbonates, there will be c. 17.6-22.0 m 3 of CO 2 present at the stabilization stage of the coking process. However, the impact of a mineral-related gas phase should not be underestimated (in particular, for porosity development and cracks formation), mostly when the grain size of the minerals is quite large. The major CO 2 -related impact on coke properties can be referred to dolomite, magnesite, and calcite.