The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach.

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The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach. / Makovicky, Emil; Topa, Dan.

I: European Journal of Mineralogy, Bind 23, Nr. 4, 07.2011, s. 537-550.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Makovicky, E & Topa, D 2011, 'The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach.', European Journal of Mineralogy, bind 23, nr. 4, s. 537-550. https://doi.org/10.1127/0935-1221/2011/0023-2114

APA

Makovicky, E., & Topa, D. (2011). The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach. European Journal of Mineralogy, 23(4), 537-550. https://doi.org/10.1127/0935-1221/2011/0023-2114

Vancouver

Makovicky E, Topa D. The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach. European Journal of Mineralogy. 2011 jul.;23(4):537-550. https://doi.org/10.1127/0935-1221/2011/0023-2114

Author

Makovicky, Emil ; Topa, Dan. / The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach. I: European Journal of Mineralogy. 2011 ; Bind 23, Nr. 4. s. 537-550.

Bibtex

@article{cfe26bfa089b495cb2503f66435c9423,
title = "The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach.",
abstract = "The crystal structure of gustavite Pb1.06Ag0.95Bi2.80Sb0.20S5.99 from Rotgu¨lden, Lungau, Salzburg Land, Austria, was refined to R1 ¼ 2.76 % using single-crystal X-ray diffraction data. Refined unit-cell parameters are a 7.0567(14), b 19.6905(39), c 8.2219(16) A ° , b 106.961(3) , unit-cell volume 1092.7(2) A ° 3 and space group is P21/c. The structure contains a bicapped trigonal prismatic Pb site, a [001] string of Ag and Bi1 octahedral sites and a similar string of Bi2 and Bi3 coordination octahedra. Sb is concentrated in the Bi3 site whereas Bi1 and Ag contain a fraction (0.1–0.14 atom) of the opposite species; the latter is explained by a presence of twin lamellae or antiphase domains in the crystal. In accordance with its frequently observed twinning, gustavite is an OD (order-disorder) structure that can be described by zig-zag unit layers with layer symmetry P(2/n) 21/c 2/m and the interlayer symmetry elements {(22/n1,1/2) 21/n1/2,2 21/2/ a2}. An alternative OD description uses planar unit layers with the layer symmetry P(2/ b) 21/c 21/m and the interlayer elements 22/n1,–1/2 21/n1/2,2 21/2/a2. The former description adheres closely to the details of coordination of bismuth observed in the structure whereas the latter description is based on a more abstract structure model.",
author = "Emil Makovicky and Dan Topa",
year = "2011",
month = jul,
doi = "10.1127/0935-1221/2011/0023-2114",
language = "English",
volume = "23",
pages = "537--550",
journal = "European Journal of Mineralogy",
issn = "0935-1221",
publisher = "E.Schweizerbart'sche Verlagsbuchhandlung",
number = "4",

}

RIS

TY - JOUR

T1 - The crystal structure of gustavite, PbAgBi3S6. Analysis of twinning and polytypism using the OD approach.

AU - Makovicky, Emil

AU - Topa, Dan

PY - 2011/7

Y1 - 2011/7

N2 - The crystal structure of gustavite Pb1.06Ag0.95Bi2.80Sb0.20S5.99 from Rotgu¨lden, Lungau, Salzburg Land, Austria, was refined to R1 ¼ 2.76 % using single-crystal X-ray diffraction data. Refined unit-cell parameters are a 7.0567(14), b 19.6905(39), c 8.2219(16) A ° , b 106.961(3) , unit-cell volume 1092.7(2) A ° 3 and space group is P21/c. The structure contains a bicapped trigonal prismatic Pb site, a [001] string of Ag and Bi1 octahedral sites and a similar string of Bi2 and Bi3 coordination octahedra. Sb is concentrated in the Bi3 site whereas Bi1 and Ag contain a fraction (0.1–0.14 atom) of the opposite species; the latter is explained by a presence of twin lamellae or antiphase domains in the crystal. In accordance with its frequently observed twinning, gustavite is an OD (order-disorder) structure that can be described by zig-zag unit layers with layer symmetry P(2/n) 21/c 2/m and the interlayer symmetry elements {(22/n1,1/2) 21/n1/2,2 21/2/ a2}. An alternative OD description uses planar unit layers with the layer symmetry P(2/ b) 21/c 21/m and the interlayer elements 22/n1,–1/2 21/n1/2,2 21/2/a2. The former description adheres closely to the details of coordination of bismuth observed in the structure whereas the latter description is based on a more abstract structure model.

AB - The crystal structure of gustavite Pb1.06Ag0.95Bi2.80Sb0.20S5.99 from Rotgu¨lden, Lungau, Salzburg Land, Austria, was refined to R1 ¼ 2.76 % using single-crystal X-ray diffraction data. Refined unit-cell parameters are a 7.0567(14), b 19.6905(39), c 8.2219(16) A ° , b 106.961(3) , unit-cell volume 1092.7(2) A ° 3 and space group is P21/c. The structure contains a bicapped trigonal prismatic Pb site, a [001] string of Ag and Bi1 octahedral sites and a similar string of Bi2 and Bi3 coordination octahedra. Sb is concentrated in the Bi3 site whereas Bi1 and Ag contain a fraction (0.1–0.14 atom) of the opposite species; the latter is explained by a presence of twin lamellae or antiphase domains in the crystal. In accordance with its frequently observed twinning, gustavite is an OD (order-disorder) structure that can be described by zig-zag unit layers with layer symmetry P(2/n) 21/c 2/m and the interlayer symmetry elements {(22/n1,1/2) 21/n1/2,2 21/2/ a2}. An alternative OD description uses planar unit layers with the layer symmetry P(2/ b) 21/c 21/m and the interlayer elements 22/n1,–1/2 21/n1/2,2 21/2/a2. The former description adheres closely to the details of coordination of bismuth observed in the structure whereas the latter description is based on a more abstract structure model.

U2 - 10.1127/0935-1221/2011/0023-2114

DO - 10.1127/0935-1221/2011/0023-2114

M3 - Journal article

VL - 23

SP - 537

EP - 550

JO - European Journal of Mineralogy

JF - European Journal of Mineralogy

SN - 0935-1221

IS - 4

ER -

ID: 36091064