NOT KNOWN FACTUAL STATEMENTS ABOUT INFRARED ZINC SULFIDE

The sphalerite construction is favored at 298k by 13kJ/mol, but at 1296K the changeover to wurtzite happens.3The discrepancies amongst minerals can be used to estimate the temperature of equilibration. The δ13C and δ34S of coexisting carbonate minerals and sulfides can be used to determine the pH and oxygen fugacity from the ore-bearing fluid for