The sphalerite construction is favored at 298k by 13kJ/mol, but at 1296K the changeover to wurtzite takes place.three The dissimilarities between minerals can be employed to estimate the temperature of equilibration. The δ13C and δ34S of coexisting carbonate minerals and sulfides may be used to ascertain the pH and oxygen https://johnl159hte6.vblogetin.com/profile