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A New Mineral Hanauerite, AgHgSI, and Common Crystal Chemical Features of Natural Mercury Sulphohalides. / Pekov, Igor V.; Zubkova, Natalia V.; Britvin, Sergey N.; Agakhanov, Atali A.; Polekhovsky, Yury S.; Pushcharovsky, Dmitry Y.; Möhn, Gerhard; Desor, Joy; Blass, Günter.

в: Crystals, Том 13, № 8, 1218, 06.08.2023.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Pekov, IV, Zubkova, NV, Britvin, SN, Agakhanov, AA, Polekhovsky, YS, Pushcharovsky, DY, Möhn, G, Desor, J & Blass, G 2023, 'A New Mineral Hanauerite, AgHgSI, and Common Crystal Chemical Features of Natural Mercury Sulphohalides', Crystals, Том. 13, № 8, 1218. https://doi.org/10.3390/cryst13081218, https://doi.org/10.3390/cryst13081218

APA

Pekov, I. V., Zubkova, N. V., Britvin, S. N., Agakhanov, A. A., Polekhovsky, Y. S., Pushcharovsky, D. Y., Möhn, G., Desor, J., & Blass, G. (2023). A New Mineral Hanauerite, AgHgSI, and Common Crystal Chemical Features of Natural Mercury Sulphohalides. Crystals, 13(8), [1218]. https://doi.org/10.3390/cryst13081218, https://doi.org/10.3390/cryst13081218

Vancouver

Author

Pekov, Igor V. ; Zubkova, Natalia V. ; Britvin, Sergey N. ; Agakhanov, Atali A. ; Polekhovsky, Yury S. ; Pushcharovsky, Dmitry Y. ; Möhn, Gerhard ; Desor, Joy ; Blass, Günter. / A New Mineral Hanauerite, AgHgSI, and Common Crystal Chemical Features of Natural Mercury Sulphohalides. в: Crystals. 2023 ; Том 13, № 8.

BibTeX

@article{6eadff530ffb4d68a74246e1d165de88,
title = "A New Mineral Hanauerite, AgHgSI, and Common Crystal Chemical Features of Natural Mercury Sulphohalides",
abstract = "A new mineral, hanauerite, ideally AgHgSI, was found in the oxidation zone of Ag- and Hg-bearing ores at two old, abandoned mines in Rhineland-Palatinate, Germany. In a holotype specimen originating from the Sch{\"o}ne Aussicht Mine, Dernbach, Westerwald, it is associated with plumbogummite–hinsdalite series of minerals and goethite. In cotype from the Friedrichssegen Mine, Bad Ems, it is associated with perroudite, goethite, and quartz. At both localities, hanauerite occurs as a prismatic crystal up to 0.15 mm long and up to 0.02 mm thick. The mineral is yellow, transparent, with an adamantine lustre. It is brittle, and cleavage was not observed. The calculated density values are 6.671 and 6.575 g cm−3 for holotype and cotype, respectively. The empirical formulae calculated (from electron microprobe data) based on the sum of all atoms = 4 apfu are Ag0.95Hg1.00S1.01(I0.83Br0.19Cl0.03)Σ1.05 for holotype and Ag0.97Hg0.97S1.05(I0.76Br0.25)Σ1.01 for cotype. Hanauerite is orthorhombic, space group Pmma; the unit cell parameters (from single-crystal X-ray diffraction data; holotype/cotype) are: a = 9.932(2)/9.9256(8), b = 4.6219(19)/4.6209(2), c = 9.891(4)/9.9006(4) {\AA}, V = 454.0(3)/454.19(5) {\AA}3, and Z = 4. The crystal structure was studied on single crystals extracted from both holotype and cotype specimens; R1 = 0.0416 (holotype) and =0.0544 (cotype). In hanauerite, Hg2+ cations centre strongly distorted octahedra with two short Hg–S bonds (Hg and S atoms build “crankshaft-type” chains) and four strongly elongated Hg–I bonds. The Hg-centred octahedra are connected via common edges and faces to form corrugated layers; Ag+ cations are located between these layers. Hanauerite is named in honour of the German mineral collector Dr. Alfred Hanauer (1912–1988). The common crystal chemical features of mercury sulphohalide minerals are discussed.",
keywords = "Friedrichssegen Mine, Sch{\"o}ne Aussicht Mine, crystal structure, hanauerite, mercury sulphohalide, new mineral, oxidation zone of ore deposit, silver mercury sulphide iodide",
author = "Pekov, {Igor V.} and Zubkova, {Natalia V.} and Britvin, {Sergey N.} and Agakhanov, {Atali A.} and Polekhovsky, {Yury S.} and Pushcharovsky, {Dmitry Y.} and Gerhard M{\"o}hn and Joy Desor and G{\"u}nter Blass",
year = "2023",
month = aug,
day = "6",
doi = "10.3390/cryst13081218",
language = "English",
volume = "13",
journal = "Crystals",
issn = "2073-4352",
publisher = "MDPI AG",
number = "8",

}

RIS

TY - JOUR

T1 - A New Mineral Hanauerite, AgHgSI, and Common Crystal Chemical Features of Natural Mercury Sulphohalides

AU - Pekov, Igor V.

AU - Zubkova, Natalia V.

AU - Britvin, Sergey N.

AU - Agakhanov, Atali A.

AU - Polekhovsky, Yury S.

AU - Pushcharovsky, Dmitry Y.

AU - Möhn, Gerhard

AU - Desor, Joy

AU - Blass, Günter

PY - 2023/8/6

Y1 - 2023/8/6

N2 - A new mineral, hanauerite, ideally AgHgSI, was found in the oxidation zone of Ag- and Hg-bearing ores at two old, abandoned mines in Rhineland-Palatinate, Germany. In a holotype specimen originating from the Schöne Aussicht Mine, Dernbach, Westerwald, it is associated with plumbogummite–hinsdalite series of minerals and goethite. In cotype from the Friedrichssegen Mine, Bad Ems, it is associated with perroudite, goethite, and quartz. At both localities, hanauerite occurs as a prismatic crystal up to 0.15 mm long and up to 0.02 mm thick. The mineral is yellow, transparent, with an adamantine lustre. It is brittle, and cleavage was not observed. The calculated density values are 6.671 and 6.575 g cm−3 for holotype and cotype, respectively. The empirical formulae calculated (from electron microprobe data) based on the sum of all atoms = 4 apfu are Ag0.95Hg1.00S1.01(I0.83Br0.19Cl0.03)Σ1.05 for holotype and Ag0.97Hg0.97S1.05(I0.76Br0.25)Σ1.01 for cotype. Hanauerite is orthorhombic, space group Pmma; the unit cell parameters (from single-crystal X-ray diffraction data; holotype/cotype) are: a = 9.932(2)/9.9256(8), b = 4.6219(19)/4.6209(2), c = 9.891(4)/9.9006(4) Å, V = 454.0(3)/454.19(5) Å3, and Z = 4. The crystal structure was studied on single crystals extracted from both holotype and cotype specimens; R1 = 0.0416 (holotype) and =0.0544 (cotype). In hanauerite, Hg2+ cations centre strongly distorted octahedra with two short Hg–S bonds (Hg and S atoms build “crankshaft-type” chains) and four strongly elongated Hg–I bonds. The Hg-centred octahedra are connected via common edges and faces to form corrugated layers; Ag+ cations are located between these layers. Hanauerite is named in honour of the German mineral collector Dr. Alfred Hanauer (1912–1988). The common crystal chemical features of mercury sulphohalide minerals are discussed.

AB - A new mineral, hanauerite, ideally AgHgSI, was found in the oxidation zone of Ag- and Hg-bearing ores at two old, abandoned mines in Rhineland-Palatinate, Germany. In a holotype specimen originating from the Schöne Aussicht Mine, Dernbach, Westerwald, it is associated with plumbogummite–hinsdalite series of minerals and goethite. In cotype from the Friedrichssegen Mine, Bad Ems, it is associated with perroudite, goethite, and quartz. At both localities, hanauerite occurs as a prismatic crystal up to 0.15 mm long and up to 0.02 mm thick. The mineral is yellow, transparent, with an adamantine lustre. It is brittle, and cleavage was not observed. The calculated density values are 6.671 and 6.575 g cm−3 for holotype and cotype, respectively. The empirical formulae calculated (from electron microprobe data) based on the sum of all atoms = 4 apfu are Ag0.95Hg1.00S1.01(I0.83Br0.19Cl0.03)Σ1.05 for holotype and Ag0.97Hg0.97S1.05(I0.76Br0.25)Σ1.01 for cotype. Hanauerite is orthorhombic, space group Pmma; the unit cell parameters (from single-crystal X-ray diffraction data; holotype/cotype) are: a = 9.932(2)/9.9256(8), b = 4.6219(19)/4.6209(2), c = 9.891(4)/9.9006(4) Å, V = 454.0(3)/454.19(5) Å3, and Z = 4. The crystal structure was studied on single crystals extracted from both holotype and cotype specimens; R1 = 0.0416 (holotype) and =0.0544 (cotype). In hanauerite, Hg2+ cations centre strongly distorted octahedra with two short Hg–S bonds (Hg and S atoms build “crankshaft-type” chains) and four strongly elongated Hg–I bonds. The Hg-centred octahedra are connected via common edges and faces to form corrugated layers; Ag+ cations are located between these layers. Hanauerite is named in honour of the German mineral collector Dr. Alfred Hanauer (1912–1988). The common crystal chemical features of mercury sulphohalide minerals are discussed.

KW - Friedrichssegen Mine

KW - Schöne Aussicht Mine

KW - crystal structure

KW - hanauerite

KW - mercury sulphohalide

KW - new mineral

KW - oxidation zone of ore deposit

KW - silver mercury sulphide iodide

UR - https://www.mendeley.com/catalogue/dbcf93de-36e5-3129-88ed-c4d04ef0f8d8/

U2 - 10.3390/cryst13081218

DO - 10.3390/cryst13081218

M3 - Article

VL - 13

JO - Crystals

JF - Crystals

SN - 2073-4352

IS - 8

M1 - 1218

ER -

ID: 113457888