“…The SiO 2 exhibits polymorphism even at atmospheric pressure and the pressure-temperature phase diagram is quite complex (for example, coesite and stishovite with densities 3 and 4.4 g cm −3 , respectively [27]). During oxide growth, especially at the initial stages studied here, most probably high pressures are created in the Si lattice as oxygen atoms are incorporated and Si interstitials emitted, if we assume a mechanism similar to that which takes place in the formation of SiO 2 precipitates in crystalline Si [28,29]. These high pressures would result in the formation of high pressure SiO 2 phases or mixture of low and high pressure phases.…”