“…Additionally, in the high‐temperature range, sulfide minerals in the copper slag, such as FeS and copper matte, react with CaO to form CaSO 4 . Due to the reactions between Fe 2 O 3 , SiO 2 , and CaO, calcium iron silicate (Ca 3 Fe 2 (SiO 4 ) 3 , PDF#77‐0119) is formed, leading to the attenuation of the SiO 2 diffraction peaks [36] …”