AN UNBIASED VIEW OF ZINC SULFIDE

The sphalerite structure is favored at 298k by 13kJ/mol, but at 1296K the transition to wurtzite happens.threeThe discrepancies concerning 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 on the ore-bearing flu