infrared zinc sulfide for Dummies
The sphalerite framework is favored at 298k by 13kJ/mol, but at 1296K the transition to wurtzite occurs.3The discrepancies in between minerals may 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