The percentage of "fayalite" in an "OLIVINE" with density 3.88 g cm−3 is:
A series of minerals consists of a crystal in which Fe2+ and Mg2+ ions may substitute for each other causing a substitutional impurity defect without changing the volume of the unit cell. In the mineral, the oxide ions exist as fcc with Si2+ occupying 14th of the octahedral voids and divalent ions occupying 14th of the tetrahedral voids. The density of forsterite (Magnesium silicate) is 3.21 g/cc and that of fayalite (Ferrous silicate) is 4.34 g/cc. If the density of mineral is 3.88 g/cc, then which of the following statements is/are CORRECT.