Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Gladkovskyite, MnTlAs3 S6, a new thallium sulfosalt from the vorontsovskoe gold deposit, Northern Urals, Russia. / Kasatkin, Anatoly V.; Makovicky, Emil; Plášil, Jakub; Škoda, Radek; Chukanov, Nikita V.; Stepanov, Sergey Y.; Agakhanov, Atali A.; Nestola, Fabrizio.
в: Journal of Geosciences (Czech Republic), Том 64, № 3, 01.01.2019, стр. 207-218.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Gladkovskyite, MnTlAs3 S6, a new thallium sulfosalt from the vorontsovskoe gold deposit, Northern Urals, Russia
AU - Kasatkin, Anatoly V.
AU - Makovicky, Emil
AU - Plášil, Jakub
AU - Škoda, Radek
AU - Chukanov, Nikita V.
AU - Stepanov, Sergey Y.
AU - Agakhanov, Atali A.
AU - Nestola, Fabrizio
PY - 2019/1/1
Y1 - 2019/1/1
N2 - Gladkovskyite (IMA2018-098), MnTlAs3 S6, is a new sulfosalt from the Vorontsovskoe gold deposit, Sverdlovsk Oblast’, Northern Urals, Russia. The new mineral occurs in limestone breccias cemented by abundant realgar, orpiment, baryte and pyrite, as well as minor clinochlore, fluorapatite, quartz and talc. Gladkovskyite forms long-prismatic crystals and grains up to 0.2 mm; it has dark cherry-red color and red streak. It is transparent with adamantine luster. The Vickers microhardness is 94 kg/mm2. The new mineral is brittle, with uneven fracture; neither cleavage nor parting was observed. The density calculated based on the empirical formula is 4.356 g/cm3. In reflected light, gladkovskyite is grayish-white, strongly anisotropic with rotation tints varying from light-grey to brown. Its pleochroism is moderate, from orange-red to dark-red, and bireflectance is very weak, ∆R = 0.58 % (589 nm). The empirical formula of gladkovskyite is Mn1.01 Tl0.99 Pb0.01 As2.86 Sb0.13 S6.00 (based on 11 atoms pfu). Prominent features in the Raman spectrum include bands of Mn–S and As–S stretching vibrations as well as numerous low-frequency bands related to phonons. Gladkovskyite is trigonal, R31c, a = 9.6392(2), c = 6.4560(15) Å, V = 519.49(12) Å3 and Z = 2. The seven strongest powder X-ray diffraction lines are [dobs, Å (I, %) (hkl) ]: 5.11 (80) (101), 4.83 (70) (110), 3.49 (50) (201), 3.23 (30) (002), 2.86 (100) (–2–11, 211), 2.68 (30) (112), 2.55 (60) (301, 202). The crystal structure of gladkovskyite was refined from the single-crystal X-ray diffraction data to R = 0.0178 for 679 observed reflections with Iobs > 3σ(I). It contains infinite chains of face-sharing MnS6 octahedra, TlS9 polyhedra and pyramidal AsS3 groups; the structure belongs to the group of seldom occurring cyclic sulfosalts. The new mineral honors Russian geologist Boris Aleksandrovich Gladkovsky who discovered the Vorontsovskoe gold deposit.
AB - Gladkovskyite (IMA2018-098), MnTlAs3 S6, is a new sulfosalt from the Vorontsovskoe gold deposit, Sverdlovsk Oblast’, Northern Urals, Russia. The new mineral occurs in limestone breccias cemented by abundant realgar, orpiment, baryte and pyrite, as well as minor clinochlore, fluorapatite, quartz and talc. Gladkovskyite forms long-prismatic crystals and grains up to 0.2 mm; it has dark cherry-red color and red streak. It is transparent with adamantine luster. The Vickers microhardness is 94 kg/mm2. The new mineral is brittle, with uneven fracture; neither cleavage nor parting was observed. The density calculated based on the empirical formula is 4.356 g/cm3. In reflected light, gladkovskyite is grayish-white, strongly anisotropic with rotation tints varying from light-grey to brown. Its pleochroism is moderate, from orange-red to dark-red, and bireflectance is very weak, ∆R = 0.58 % (589 nm). The empirical formula of gladkovskyite is Mn1.01 Tl0.99 Pb0.01 As2.86 Sb0.13 S6.00 (based on 11 atoms pfu). Prominent features in the Raman spectrum include bands of Mn–S and As–S stretching vibrations as well as numerous low-frequency bands related to phonons. Gladkovskyite is trigonal, R31c, a = 9.6392(2), c = 6.4560(15) Å, V = 519.49(12) Å3 and Z = 2. The seven strongest powder X-ray diffraction lines are [dobs, Å (I, %) (hkl) ]: 5.11 (80) (101), 4.83 (70) (110), 3.49 (50) (201), 3.23 (30) (002), 2.86 (100) (–2–11, 211), 2.68 (30) (112), 2.55 (60) (301, 202). The crystal structure of gladkovskyite was refined from the single-crystal X-ray diffraction data to R = 0.0178 for 679 observed reflections with Iobs > 3σ(I). It contains infinite chains of face-sharing MnS6 octahedra, TlS9 polyhedra and pyramidal AsS3 groups; the structure belongs to the group of seldom occurring cyclic sulfosalts. The new mineral honors Russian geologist Boris Aleksandrovich Gladkovsky who discovered the Vorontsovskoe gold deposit.
KW - Crystal structure
KW - Gladkovskyite
KW - New mineral
KW - Northern Urals
KW - Sulfosalt
KW - Vorontsovskoe gold deposit
KW - sulfosalt
KW - CRYSTAL-STRUCTURES
KW - REALGAR
KW - new mineral
KW - SULFIDE
KW - REFINEMENT
KW - gladkovskyite
KW - MINERALIZATION
KW - crystal structure
KW - TL
KW - GEOCHEMISTRY
KW - SPECTRA
UR - http://www.scopus.com/inward/record.url?scp=85075305211&partnerID=8YFLogxK
U2 - 10.3190/jgeosci.290
DO - 10.3190/jgeosci.290
M3 - Article
AN - SCOPUS:85075305211
VL - 64
SP - 207
EP - 218
JO - Journal of Geosciences
JF - Journal of Geosciences
SN - 1802-6222
IS - 3
ER -
ID: 49873933