The sphalerite structure is favored at 298k by 13kJ/mol, but at 1296K the transition to wurtzite happens.three The differences in between minerals may be used to estimate the temperature of equilibration. The δ13C and δ34S of coexisting carbonate minerals and sulfides can be employed to find out the pH and https://infraredzincsulfide74951.glifeblog.com/27626425/zinc-sulfide-for-dummies