“…It is evident that β-quartz which is introduced by quartz sand is consumed to form the malayaite phase. Furthermore, starting from 1,250°С, a set of absorption bands typical for tin sphene (Zhang et al , 1999; Lee and Lee, 2009; Lee et al , 2009; Cordoncillo et al , 2009; Lopez-Navarrete et al , 2003; Lopez-Navarrete and Ocana, 2002) is recorded. These bands reach maximum intensity after firing at the temperature of 1,350°С.…”