This study assesses the displacement of coalbed methane by CO 2 migration along a fault into the coal seam in the Yaojie coalfield. Coal and gas samples were collected continuously at various distances in NO.2 coal seam from F19 fault. Vitrinite reflectance, maceral, and pore distributions and proximate analysis of fourteen coal samples were performed. Gas components, concentrations, carbon isotopes of 28 gas samples were determined. We examined the coal-gas trace characteristics of coalbed methane displaced away from the fault by CO 2 injection after geological ages. From east to west, away from the F19 fault, the CO 2 concentration decreased, whereas the CH 4 concentration increased gradually. The d 13 C values for CO 2 varied between À9.94& and 1.12&, suggesting a metamorphic origin. A wider range of d 13 C CO2 values (from À9.94& to 20&) was associated with the mixing of microbial carbon dioxide, isotopic fractionation during CO 2 migration through the microporous structures of coals, and/or carbon isotope fractionation during gas-water exchange and dissolution of CO 2 . Away from the F19 fault, the volumes of micropores, mesopores and macropores decrease gradually. The Dubinin-Radushkevich (DR) micropore volume decreased from 0.0059 to 0.0037 cm 3 g -1 , and the mesopore and macropore volumes decreased from 0.066 to 0.026 cm 3 g -1 . The CO 2 injection can mobilize aromatic hydrocarbons and mineral matter from coal matrix, resulting in the decrease in the absorption peak intensity for coal samples after supercritical CO 2 treatment, which indicates that chemical reactions occur between coal and CO 2 , not only physical adsorption.