ŠTUBŇA, Ján, Peter BAČÍK, Jana FRIDRICHOVÁ, Radek HANUS, Ľudmila ILLÁŠOVÁ, Stanislava MILOVSKÁ, Radek ŠKODA, Tomáš VACULOVIČ and Slavomír ČERŇANSKÝ. Gem-Quality Green Cr-Bearing Andradite (var. Demantoid) from Dobsina, Slovakia. Minerals. Basel: MDPI, 2019, vol. 9, No 3, p. 1-12. ISSN 2075-163X. Available from: https://dx.doi.org/10.3390/min9030164.
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Basic information
Original name Gem-Quality Green Cr-Bearing Andradite (var. Demantoid) from Dobsina, Slovakia
Authors ŠTUBŇA, Ján (703 Slovakia, guarantor), Peter BAČÍK, Jana FRIDRICHOVÁ, Radek HANUS, Ľudmila ILLÁŠOVÁ, Stanislava MILOVSKÁ, Radek ŠKODA (203 Czech Republic, belonging to the institution), Tomáš VACULOVIČ (203 Czech Republic, belonging to the institution) and Slavomír ČERŇANSKÝ.
Edition Minerals, Basel, MDPI, 2019, 2075-163X.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10504 Mineralogy
Country of publisher Switzerland
Confidentiality degree is not subject to a state or trade secret
WWW Full Text
Impact factor Impact factor: 2.380
RIV identification code RIV/00216224:14310/19:00111294
Organization unit Faculty of Science
Doi http://dx.doi.org/10.3390/min9030164
UT WoS 000464443000002
Keywords in English andradite; demantoid; gemstone; Raman spectroscopy; UV-Vis-NIR spectroscopy; X-ray fluorescence spectroscopy; gem-quality; garnet
Tags rivok
Tags International impact, Reviewed
Changed by Changed by: Mgr. Marie Šípková, DiS., učo 437722. Changed: 26/3/2020 13:40.
Abstract
Andradite, variety demantoid, is a rare gem mineral. We describe gem-quality garnet crystals from serpentinized harzburgites from Dobsina, Slovakia which were faceted. Both the andradite samples were transparent, with a vitreous luster and a vivid green color. They were isotropic with refractive indices >1.81. The measured density ranged from 3.82 to 3.84 g center dot cm(-3). Andradite var. demantoid appeared red under Chelsea filter observation. Both samples contained fibrous crystalline inclusions with the typical "horsetail" arrangement. The studied garnet had a strong Fe3+ dominant andradite composition with 1.72-1.85 apfu Fe3+, Cr3+ up to 0.15 apfu, Al3+ 0.03 to 0.04 apfu, V3+ up to 0.006 apfu substituted for Fe3+, Mn2+ up to 0.002 apfu, and Mg up to 0.04 apfu substituted for Ca. Raman spectrum of garnet showed three spectral regions containing relatively strong bands: I-352-371 cm(-1), II-816-874 cm(-1), and III-493-516 cm(-1). The optical absorption spectrum as characterized by an intense band at 438 nm and two broad bands at 587 and 623 nm and last one at 861 nm, which were assigned to Fe3+ and Cr3+. Transmission was observed in the ultraviolet spectral region (<390 nm), near the infrared region (700-800 nm), and around 530 nm in the green region of visible light, resulting in the garnet's green color.
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