infrared zinc sulfide Fundamentals Explained
The sphalerite composition is favored at 298k by 13kJ/mol, but at 1296K the transition to wurtzite happens.3The discrepancies amongst minerals can be utilized to estimate the temperature of equilibration. The δ13C and δ34S of coexisting carbonate minerals and sulfides can be utilized to find out the pH and oxygen fugacity in the ore-bearing fluid