Large Cat’s-Eye Emerald from Brazil
Gübelin Gem Laboratories (GGL) in Hong Kong and
Lucerne recently had the opportunity to examine a translucent emerald,
weighing approximately 43 ct, that exhibited a pronounced and
well-centered chatoyancy (figure 1). The stone had a spot RI of 1.57 and
a hydrostatic SG of 2.73, and it was inert under long- and short-wave
UV radiation. Microscopic observation in reflected and transmitted light
presented a series of dense elongated, rectangular, and square
multiphase inclusions (figure 2).
The UV-Vis absorption spectra showed the characteristic Cr3+- as well as Fe2+- and Fe3+- related bands. In the FTIR absorption spectra, type I and type II water molecules were observed. An intense band at around 2360 cm–1 indicated the presence of CO2, most likely in the multiphase inclusions. Trace-element analysis of the sample with laser ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) showed contents consistent with schist- and pegmatite-related emeralds. It also showed lower Li, Cs, and Rb than in emeralds related to highly evolved pegmatites, such as those from Sandawana (Zimbabwe) and Kafubu (Zambia); see J.C. Zwaan et al., “Emeralds from the Fazenda Bonfim region, Rio Grande do Norte, Brazil,” Spring 2012 G&G, pp. 2–17. The stone’s composition was consistent with emeralds from Itabira–Nova Era, Minas Gerais, based on GGL’s reference collection and the published literature on the pegmatites of the area (C. Preinfalk et al., “The pegmatites of the Nova Era–Itabira–Ferros pegmatite district and the emerald mineralisation of Capoeirana and Belmont (Minas Gerais, Brazil): geochemistry and Rb-Sr dating,” Journal of South American Sciences, Vol. 14, No. 8, 2002, pp. 867–887). This exceptional stone is one of the largest Brazilian cat’s-eye emeralds examined by GGL to date.
The UV-Vis absorption spectra showed the characteristic Cr3+- as well as Fe2+- and Fe3+- related bands. In the FTIR absorption spectra, type I and type II water molecules were observed. An intense band at around 2360 cm–1 indicated the presence of CO2, most likely in the multiphase inclusions. Trace-element analysis of the sample with laser ablation–inductively coupled plasma–mass spectrometry (LA-ICP-MS) showed contents consistent with schist- and pegmatite-related emeralds. It also showed lower Li, Cs, and Rb than in emeralds related to highly evolved pegmatites, such as those from Sandawana (Zimbabwe) and Kafubu (Zambia); see J.C. Zwaan et al., “Emeralds from the Fazenda Bonfim region, Rio Grande do Norte, Brazil,” Spring 2012 G&G, pp. 2–17. The stone’s composition was consistent with emeralds from Itabira–Nova Era, Minas Gerais, based on GGL’s reference collection and the published literature on the pegmatites of the area (C. Preinfalk et al., “The pegmatites of the Nova Era–Itabira–Ferros pegmatite district and the emerald mineralisation of Capoeirana and Belmont (Minas Gerais, Brazil): geochemistry and Rb-Sr dating,” Journal of South American Sciences, Vol. 14, No. 8, 2002, pp. 867–887). This exceptional stone is one of the largest Brazilian cat’s-eye emeralds examined by GGL to date.
Nenhum comentário:
Postar um comentário