The olivine series of minerals consists of crystal in which Fe2+ and Mg2+ ions may substitute for each-other causing substitutional impurity defect without changing the volume of the unit cell. In olivine series of mineral, oxide ion exists as fcc with Si4+ occupying 14th of the octahedral void and divalent ion occupying 14th th of the tetrahedral void. The density of forsterite (Magnesium silicate) is 3.0 g/cc and that of fayalite (Ferrous silicate) is 4.0 g/cc. If density of olivine is 3.53 g/cc, then which of the following statement is INCORRECT.