The increasing atmospheric CO₂ concentration linked to human activity results in global warming by the greenhouse effect. This anthropogenic CO₂ may be sequestrated into geological formations, e.g., porous basalts, saline aquifers, depleted oil or gas reservoirs, and unmineable coal seams. Furthermore, carbon capture, utilization, and storage (CCUS) methods are an acceptable and sustainable technology to meet the goals of the Paris Agreement, in which Kazakhstan is expected to reduce greenhouse gas emissions by 25% compared with the 1990 level. Unmineable coal seams are an attractive option among all geostorage solutions, as CO₂ sequestration in coal comes with an income stream via enhanced coalbed methane (ECBM) recovery. This paper identifies four carboniferous coal formations, namely Karagandy, Teniz-Korzhinkol, Ekibustuz, and Chu coal basins of Kazakhstan, as CO₂ geostorage solutions for their unmineable coal seams. The ideal depth of CO₂ storage is identified as 800 m to ensure the supercritical state of CO₂. However, the Ekibustuz coal basin fails to meet the required depth of 800 m in its unmineable coal seams. The conventional formula for calculating CO₂ storage in coal basins has been modified, and a new formula has been proposed for assessing the CO₂ storage potential in a coal seam. The CO₂ storage capacities of unmineable coal seam of these coal basins are 24.60 Bt, 0.61 Bt, 14.02 Bt, and 5.42 Bt, respectively. The Langmuir volume of the coal fields was calculated using the proximate analysis of coalfields and found to vary between 36.42 and 98.90 m³/ton. This paper is the first to outline CO₂ storage potential in Kazakhstani coal basins, albeit with limited data, along with a detailed geological and paleographic review of the carboniferous coalfields of Kazakhstan. A short overview of the CO₂-ECBM process was also included in the paper. Instead of any experimental work for CO₂ storage, this paper attempts to present the CO₂ storage capacity of carboniferous coal formation using the modified version of previously determined formulas for CO₂ storage.