Results CL
CL clearly documents that the corundum crystal has a homogeneous red luminescing core and a slightly brighter luminescing outer zone of similar thickness (
Fig. 53).
Between the core and the outer zone, a transitional boundary exists with a lower luminescence intensity than the outer zone (
Fig. 51 and
Fig. 53). The red CL from both areas contains identical peaks, with peak positions indicative for Cr
3+-induced luminescence (
Fig. 52). LA-ICP-MS data confirms the presence of Cr but also Mg, Fe, Ti, Be and Ga are present (
Fig. 53). As shown by LA-ICP-MS, a depletion of the elements Mg, Fe, Ti, Cr, and Ga is found in the outer zone of this sample and Beryllium is enriched.
The outer zone was formed after crystallization and reshaping of the crystal and thus represents the result of a treatment.
Further investigation on the interpretation of the CL data are in preparation (Ramseyer, Peretti and Mullis, in prep.).