Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral

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Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral. / Biagioni, Cristian; Sejkora, Jiří; Musetti, Silvia; Makovicky, Emil; Pagano, Renato; Pasero, Marco; Dolníček, Zdeněk.

I: Mineralogical Magazine, Bind 86, Nr. 1, 2022, s. 168-175.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Biagioni, C, Sejkora, J, Musetti, S, Makovicky, E, Pagano, R, Pasero, M & Dolníček, Z 2022, 'Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral', Mineralogical Magazine, bind 86, nr. 1, s. 168-175. https://doi.org/10.1180/mgm.2021.107

APA

Biagioni, C., Sejkora, J., Musetti, S., Makovicky, E., Pagano, R., Pasero, M., & Dolníček, Z. (2022). Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral. Mineralogical Magazine, 86(1), 168-175. https://doi.org/10.1180/mgm.2021.107

Vancouver

Biagioni C, Sejkora J, Musetti S, Makovicky E, Pagano R, Pasero M o.a. Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral. Mineralogical Magazine. 2022;86(1):168-175. https://doi.org/10.1180/mgm.2021.107

Author

Biagioni, Cristian ; Sejkora, Jiří ; Musetti, Silvia ; Makovicky, Emil ; Pagano, Renato ; Pasero, Marco ; Dolníček, Zdeněk. / Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral. I: Mineralogical Magazine. 2022 ; Bind 86, Nr. 1. s. 168-175.

Bibtex

@article{1c69afd29cd844dfbad57ea68709c3e4,
title = "Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral",
abstract = "Stibiogoldfieldite, Cu12(Sb2Te2)S13, was approved as a new mineral species from the Mohawk mine, Goldfield mining district, Esmeralda County, Nevada, USA. It occurs as metallic anhedral grains, dark grey in colour. It is associated with quartz, pyrite and an Ag-Bi-(S,Se) phase (holotype material) and with quartz, pyrite, calaverite, bismuthinite, bohdanowiczite, and the Ag-Bi-(S,Se) phase (cotype material). In reflected light, stibiogoldfieldite is isotropic, grey in colour, with indistinct brownish shade. Reflectance data in air [R (%)] are: 31.1 at 470 nm, 30.9 at 546 nm, 30.8 at 589 nm and 31.0 at 650 nm. Electron microprobe analysis for holotype material gave (in wt.% - average of 60 spot analyses): Cu 45.03(60), Ag 0.26(7), Fe 0.02(3), Zn 0.13(15), Sn 0.02(4), Pb 0.05(6), Sb 8.02(62), As 2.80(65), Bi 2.77(87), Te 15.15(1.24), S 24.50(32), Se 0.52(11), total 99.27(69). On the basis of (As + Sb + Te + Bi) = 4 atoms per formula unit (apfu), the empirical formula of stibiogoldfieldite is (Cu12.05Ag0.04Zn0.03Fe0.01)Σ12.13(Sb1.12As0.63Bi0.23Te2.02)Σ4.00(S12.99Se0.11)Σ13.10. Chemical data on an additional sample from the same locality (cotype material) gave the following results (in wt.% - average of 181 spot analyses): Cu 43.84(63), Ag 0.21(7), Sb 5.92(78), As 2.63(45), Te 20.07(1.19), S 25.13(53), Se 0.97(35), total 99.47(66). On the basis of (As + Sb + Te + Bi) = 4 apfu, the empirical formula of cotype material is (Cu11.30Ag0.03)Σ11.33(Sb0.80As0.57Bi0.06Te2.57)Σ4.00(S12.83Se0.20)Σ13.03. Stibiogoldfieldite is cubic, IFormula Presented3m, with unit-cell parameters a = 10.3466(17) {\AA}, V = 1107.6(5) {\AA}3 and Z = 2 (holotype). Unit-cell parameters for the cotype sample are a = 10.3035(2) {\AA} and V = 1093.83(7) {\AA}3. The crystal structure of holotype stibiogoldfieldite was refined by single-crystal X-ray diffraction data to a final R1 = 0.032 on the basis of 285 reflections with Fo > 4σ(Fo) and 20 refined parameters. Stibiogoldfieldite is isotypic with other members of the tetrahedrite group.",
keywords = "antimony, copper, crystal structure, Goldfield mining district, Nevada, new mineral, stibiogoldfieldite, sulfosalt, tellurium, USA",
author = "Cristian Biagioni and Ji{\v r}{\'i} Sejkora and Silvia Musetti and Emil Makovicky and Renato Pagano and Marco Pasero and Zden{\v e}k Doln{\'i}{\v c}ek",
note = "Publisher Copyright: Copyright {\textcopyright} The Author(s), 2022. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland.",
year = "2022",
doi = "10.1180/mgm.2021.107",
language = "English",
volume = "86",
pages = "168--175",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "1",

}

RIS

TY - JOUR

T1 - Stibiogoldfieldite, Cu12(Sb2Te2)S13, a new tetrahedrite-group mineral

AU - Biagioni, Cristian

AU - Sejkora, Jiří

AU - Musetti, Silvia

AU - Makovicky, Emil

AU - Pagano, Renato

AU - Pasero, Marco

AU - Dolníček, Zdeněk

N1 - Publisher Copyright: Copyright © The Author(s), 2022. Published by Cambridge University Press on behalf of The Mineralogical Society of Great Britain and Ireland.

PY - 2022

Y1 - 2022

N2 - Stibiogoldfieldite, Cu12(Sb2Te2)S13, was approved as a new mineral species from the Mohawk mine, Goldfield mining district, Esmeralda County, Nevada, USA. It occurs as metallic anhedral grains, dark grey in colour. It is associated with quartz, pyrite and an Ag-Bi-(S,Se) phase (holotype material) and with quartz, pyrite, calaverite, bismuthinite, bohdanowiczite, and the Ag-Bi-(S,Se) phase (cotype material). In reflected light, stibiogoldfieldite is isotropic, grey in colour, with indistinct brownish shade. Reflectance data in air [R (%)] are: 31.1 at 470 nm, 30.9 at 546 nm, 30.8 at 589 nm and 31.0 at 650 nm. Electron microprobe analysis for holotype material gave (in wt.% - average of 60 spot analyses): Cu 45.03(60), Ag 0.26(7), Fe 0.02(3), Zn 0.13(15), Sn 0.02(4), Pb 0.05(6), Sb 8.02(62), As 2.80(65), Bi 2.77(87), Te 15.15(1.24), S 24.50(32), Se 0.52(11), total 99.27(69). On the basis of (As + Sb + Te + Bi) = 4 atoms per formula unit (apfu), the empirical formula of stibiogoldfieldite is (Cu12.05Ag0.04Zn0.03Fe0.01)Σ12.13(Sb1.12As0.63Bi0.23Te2.02)Σ4.00(S12.99Se0.11)Σ13.10. Chemical data on an additional sample from the same locality (cotype material) gave the following results (in wt.% - average of 181 spot analyses): Cu 43.84(63), Ag 0.21(7), Sb 5.92(78), As 2.63(45), Te 20.07(1.19), S 25.13(53), Se 0.97(35), total 99.47(66). On the basis of (As + Sb + Te + Bi) = 4 apfu, the empirical formula of cotype material is (Cu11.30Ag0.03)Σ11.33(Sb0.80As0.57Bi0.06Te2.57)Σ4.00(S12.83Se0.20)Σ13.03. Stibiogoldfieldite is cubic, IFormula Presented3m, with unit-cell parameters a = 10.3466(17) Å, V = 1107.6(5) Å3 and Z = 2 (holotype). Unit-cell parameters for the cotype sample are a = 10.3035(2) Å and V = 1093.83(7) Å3. The crystal structure of holotype stibiogoldfieldite was refined by single-crystal X-ray diffraction data to a final R1 = 0.032 on the basis of 285 reflections with Fo > 4σ(Fo) and 20 refined parameters. Stibiogoldfieldite is isotypic with other members of the tetrahedrite group.

AB - Stibiogoldfieldite, Cu12(Sb2Te2)S13, was approved as a new mineral species from the Mohawk mine, Goldfield mining district, Esmeralda County, Nevada, USA. It occurs as metallic anhedral grains, dark grey in colour. It is associated with quartz, pyrite and an Ag-Bi-(S,Se) phase (holotype material) and with quartz, pyrite, calaverite, bismuthinite, bohdanowiczite, and the Ag-Bi-(S,Se) phase (cotype material). In reflected light, stibiogoldfieldite is isotropic, grey in colour, with indistinct brownish shade. Reflectance data in air [R (%)] are: 31.1 at 470 nm, 30.9 at 546 nm, 30.8 at 589 nm and 31.0 at 650 nm. Electron microprobe analysis for holotype material gave (in wt.% - average of 60 spot analyses): Cu 45.03(60), Ag 0.26(7), Fe 0.02(3), Zn 0.13(15), Sn 0.02(4), Pb 0.05(6), Sb 8.02(62), As 2.80(65), Bi 2.77(87), Te 15.15(1.24), S 24.50(32), Se 0.52(11), total 99.27(69). On the basis of (As + Sb + Te + Bi) = 4 atoms per formula unit (apfu), the empirical formula of stibiogoldfieldite is (Cu12.05Ag0.04Zn0.03Fe0.01)Σ12.13(Sb1.12As0.63Bi0.23Te2.02)Σ4.00(S12.99Se0.11)Σ13.10. Chemical data on an additional sample from the same locality (cotype material) gave the following results (in wt.% - average of 181 spot analyses): Cu 43.84(63), Ag 0.21(7), Sb 5.92(78), As 2.63(45), Te 20.07(1.19), S 25.13(53), Se 0.97(35), total 99.47(66). On the basis of (As + Sb + Te + Bi) = 4 apfu, the empirical formula of cotype material is (Cu11.30Ag0.03)Σ11.33(Sb0.80As0.57Bi0.06Te2.57)Σ4.00(S12.83Se0.20)Σ13.03. Stibiogoldfieldite is cubic, IFormula Presented3m, with unit-cell parameters a = 10.3466(17) Å, V = 1107.6(5) Å3 and Z = 2 (holotype). Unit-cell parameters for the cotype sample are a = 10.3035(2) Å and V = 1093.83(7) Å3. The crystal structure of holotype stibiogoldfieldite was refined by single-crystal X-ray diffraction data to a final R1 = 0.032 on the basis of 285 reflections with Fo > 4σ(Fo) and 20 refined parameters. Stibiogoldfieldite is isotypic with other members of the tetrahedrite group.

KW - antimony

KW - copper

KW - crystal structure

KW - Goldfield mining district

KW - Nevada

KW - new mineral

KW - stibiogoldfieldite

KW - sulfosalt

KW - tellurium

KW - USA

U2 - 10.1180/mgm.2021.107

DO - 10.1180/mgm.2021.107

M3 - Journal article

AN - SCOPUS:85123068353

VL - 86

SP - 168

EP - 175

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 1

ER -

ID: 342675753