The infrared zinc sulfide Diaries
The sphalerite structure is favored at 298k by 13kJ/mol, but at 1296K the changeover to wurtzite happens.threeThe distinctions among minerals can be used to estimate the temperature of equilibration. The δ13C and δ34S of coexisting carbonate minerals and sulfides can be utilized to determine the pH and oxygen fugacity from the ore-bearing fluid i