THE 5-SECOND TRICK FOR INFRARED ZINC SULFIDE

The sphalerite structure is favored at 298k by 13kJ/mol, but at 1296K the changeover to wurtzite happens.3The differences amongst minerals may be used to estimate the temperature of equilibration. The δ13C and δ34S of coexisting carbonate minerals and sulfides can be used to ascertain the pH and oxygen fugacity of your ore-bearing fluid through o