Standard

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 изданияхстатьяРецензирование

Harvard

Kasatkin, AV, Makovicky, E, Plášil, J, Škoda, R, Chukanov, NV, Stepanov, SY, Agakhanov, AA & Nestola, F 2019, 'Gladkovskyite, MnTlAs3 S6, a new thallium sulfosalt from the vorontsovskoe gold deposit, Northern Urals, Russia', Journal of Geosciences (Czech Republic), Том. 64, № 3, стр. 207-218. https://doi.org/10.3190/jgeosci.290

APA

Kasatkin, A. V., Makovicky, E., Plášil, J., Škoda, R., Chukanov, N. V., Stepanov, S. Y., Agakhanov, A. A., & Nestola, F. (2019). Gladkovskyite, MnTlAs3 S6, a new thallium sulfosalt from the vorontsovskoe gold deposit, Northern Urals, Russia. Journal of Geosciences (Czech Republic), 64(3), 207-218. https://doi.org/10.3190/jgeosci.290

Vancouver

Kasatkin AV, Makovicky E, Plášil J, Škoda R, Chukanov NV, Stepanov SY и пр. Gladkovskyite, MnTlAs3 S6, a new thallium sulfosalt from the vorontsovskoe gold deposit, Northern Urals, Russia. Journal of Geosciences (Czech Republic). 2019 Янв. 1;64(3):207-218. https://doi.org/10.3190/jgeosci.290

Author

Kasatkin, Anatoly V. ; Makovicky, Emil ; Plášil, Jakub ; Škoda, Radek ; Chukanov, Nikita V. ; Stepanov, Sergey Y. ; Agakhanov, Atali A. ; Nestola, Fabrizio. / Gladkovskyite, MnTlAs3 S6, a new thallium sulfosalt from the vorontsovskoe gold deposit, Northern Urals, Russia. в: Journal of Geosciences (Czech Republic). 2019 ; Том 64, № 3. стр. 207-218.

BibTeX

@article{ddd427c4ae9e47218724c6b40ff75fdc,
title = "Gladkovskyite, MnTlAs3 S6, a new thallium sulfosalt from the vorontsovskoe gold deposit, Northern Urals, Russia",
abstract = "Gladkovskyite (IMA2018-098), MnTlAs3 S6, is a new sulfosalt from the Vorontsovskoe gold deposit, Sverdlovsk Oblast{\textquoteright}, 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) {\AA}, V = 519.49(12) {\AA}3 and Z = 2. The seven strongest powder X-ray diffraction lines are [dobs, {\AA} (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.",
keywords = "Crystal structure, Gladkovskyite, New mineral, Northern Urals, Sulfosalt, Vorontsovskoe gold deposit, sulfosalt, CRYSTAL-STRUCTURES, REALGAR, new mineral, SULFIDE, REFINEMENT, gladkovskyite, MINERALIZATION, crystal structure, TL, GEOCHEMISTRY, SPECTRA",
author = "Kasatkin, {Anatoly V.} and Emil Makovicky and Jakub Pl{\'a}{\v s}il and Radek {\v S}koda and Chukanov, {Nikita V.} and Stepanov, {Sergey Y.} and Agakhanov, {Atali A.} and Fabrizio Nestola",
year = "2019",
month = jan,
day = "1",
doi = "10.3190/jgeosci.290",
language = "English",
volume = "64",
pages = "207--218",
journal = "Journal of Geosciences",
issn = "1802-6222",
publisher = "Czech Geological Survey",
number = "3",

}

RIS

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