“…These results may indicate migration of atoms present in the sample, through different phases, as identified by microprobe analysis ͑WDX͒, such as quartz and mica, besides alexandrite. Alexandrite optical absorption has been extensively presented in the literature from 4 K to 300 K ͑Powell et al, 1985;Liu et al, 1995;Walling et al, 1985;Zhang et al, 1993͒. These spectra show two narrow lines close to 680 nm, called R lines, which are identified as Cr 3ϩ lines, associated with ions at sites located on a reflection plane ͑Al 2 sites͒.…”