First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy): Chemical data and single- crystal X-ray study

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First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy) : Chemical data and single- crystal X-ray study. / Pinto, Daniela; Balic-Zunic, Tonci; Garavelli, anna; Garbarino, Carlo; Makovicky, Emil; Vurro, Filippo.

I: European Journal of Mineralogy, Bind 18, Nr. 3, 2006, s. 393-401.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Pinto, D, Balic-Zunic, T, Garavelli, A, Garbarino, C, Makovicky, E & Vurro, F 2006, 'First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy): Chemical data and single- crystal X-ray study', European Journal of Mineralogy, bind 18, nr. 3, s. 393-401. https://doi.org/1221/2006/0018-0393

APA

Pinto, D., Balic-Zunic, T., Garavelli, A., Garbarino, C., Makovicky, E., & Vurro, F. (2006). First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy): Chemical data and single- crystal X-ray study. European Journal of Mineralogy, 18(3), 393-401. https://doi.org/1221/2006/0018-0393

Vancouver

Pinto D, Balic-Zunic T, Garavelli A, Garbarino C, Makovicky E, Vurro F. First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy): Chemical data and single- crystal X-ray study. European Journal of Mineralogy. 2006;18(3):393-401. https://doi.org/1221/2006/0018-0393

Author

Pinto, Daniela ; Balic-Zunic, Tonci ; Garavelli, anna ; Garbarino, Carlo ; Makovicky, Emil ; Vurro, Filippo. / First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy) : Chemical data and single- crystal X-ray study. I: European Journal of Mineralogy. 2006 ; Bind 18, Nr. 3. s. 393-401.

Bibtex

@article{ad27dd7074c211dbbee902004c4f4f50,
title = "First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy): Chemical data and single- crystal X-ray study",
abstract = "Samples of kirkiite from the high temperature fumaroles of La Fossa crater of Vulcano (Aeolian islands, Italy) were chemically and structurally investigated in this work. Associated minerals are vurroite, bismuthinite, galenobismutite, cannizzarite, lillianite, heyrovskite, galena, and other less characterized Pb(Bi)-sulfochlorides. Electron-microprobe analyses gave the average chemical formula Pb10.00Bi3.01As3.01(S18.47Se0.44C10.06) which is very close to the ideal composition of kirkiite, Pb10Bi3As3S19, and indeed significantly closer than the composition of the type specimen, Pb10.08Bi2.55Sb0.13As2.91S19. Lattice parameters are: a = 8.700(2) {\AA}, {\ss} = 26.237(6) {\AA}, c = 8.774(3) {\AA}, {\ss} = 119.653(4)°, V = 1740.2(9) {\AA}3. A twinned structure was refined using single-crystal data (MoK X-ray diffraction, CCD detector). The refinement converges to R = 0.074 for 1443 reflections with F0 > 4(F0). The structure of the close-to-ideal kirkiite from Vulcano has been compared with the structure of the type specimen. The comparison reveals a variation in As-Bi substitution, with samples from Vulcano probably being close to the maximum possible Bi and the minimum As content for this structure type. This is reflected in more regular and symmetric coordination polyhedra than in the holotype, as well as in the overall regularity of the structure. The increased Bi:As ratio produces an elongation of the a and b lattice periods, and a shortening of the c period, and increases the frequency of twinning in kirkiite. ",
keywords = "Faculty of Science, Kirkiite, krystal strukturer, sulfosalte, kirkiite, Vulcano fumaroles, twinning, crystal structure, sulfosalts",
author = "Daniela Pinto and Tonci Balic-Zunic and anna Garavelli and Carlo Garbarino and Emil Makovicky and Filippo Vurro",
year = "2006",
doi = "1221/2006/0018-0393",
language = "English",
volume = "18",
pages = "393--401",
journal = "European Journal of Mineralogy",
issn = "0935-1221",
publisher = "E.Schweizerbart'sche Verlagsbuchhandlung",
number = "3",

}

RIS

TY - JOUR

T1 - First occurrence of close-to-ideal Kirkiite at Vulcano (Aeolian Islands, Italy)

T2 - Chemical data and single- crystal X-ray study

AU - Pinto, Daniela

AU - Balic-Zunic, Tonci

AU - Garavelli, anna

AU - Garbarino, Carlo

AU - Makovicky, Emil

AU - Vurro, Filippo

PY - 2006

Y1 - 2006

N2 - Samples of kirkiite from the high temperature fumaroles of La Fossa crater of Vulcano (Aeolian islands, Italy) were chemically and structurally investigated in this work. Associated minerals are vurroite, bismuthinite, galenobismutite, cannizzarite, lillianite, heyrovskite, galena, and other less characterized Pb(Bi)-sulfochlorides. Electron-microprobe analyses gave the average chemical formula Pb10.00Bi3.01As3.01(S18.47Se0.44C10.06) which is very close to the ideal composition of kirkiite, Pb10Bi3As3S19, and indeed significantly closer than the composition of the type specimen, Pb10.08Bi2.55Sb0.13As2.91S19. Lattice parameters are: a = 8.700(2) Å, ß = 26.237(6) Å, c = 8.774(3) Å, ß = 119.653(4)°, V = 1740.2(9) Å3. A twinned structure was refined using single-crystal data (MoK X-ray diffraction, CCD detector). The refinement converges to R = 0.074 for 1443 reflections with F0 > 4(F0). The structure of the close-to-ideal kirkiite from Vulcano has been compared with the structure of the type specimen. The comparison reveals a variation in As-Bi substitution, with samples from Vulcano probably being close to the maximum possible Bi and the minimum As content for this structure type. This is reflected in more regular and symmetric coordination polyhedra than in the holotype, as well as in the overall regularity of the structure. The increased Bi:As ratio produces an elongation of the a and b lattice periods, and a shortening of the c period, and increases the frequency of twinning in kirkiite.

AB - Samples of kirkiite from the high temperature fumaroles of La Fossa crater of Vulcano (Aeolian islands, Italy) were chemically and structurally investigated in this work. Associated minerals are vurroite, bismuthinite, galenobismutite, cannizzarite, lillianite, heyrovskite, galena, and other less characterized Pb(Bi)-sulfochlorides. Electron-microprobe analyses gave the average chemical formula Pb10.00Bi3.01As3.01(S18.47Se0.44C10.06) which is very close to the ideal composition of kirkiite, Pb10Bi3As3S19, and indeed significantly closer than the composition of the type specimen, Pb10.08Bi2.55Sb0.13As2.91S19. Lattice parameters are: a = 8.700(2) Å, ß = 26.237(6) Å, c = 8.774(3) Å, ß = 119.653(4)°, V = 1740.2(9) Å3. A twinned structure was refined using single-crystal data (MoK X-ray diffraction, CCD detector). The refinement converges to R = 0.074 for 1443 reflections with F0 > 4(F0). The structure of the close-to-ideal kirkiite from Vulcano has been compared with the structure of the type specimen. The comparison reveals a variation in As-Bi substitution, with samples from Vulcano probably being close to the maximum possible Bi and the minimum As content for this structure type. This is reflected in more regular and symmetric coordination polyhedra than in the holotype, as well as in the overall regularity of the structure. The increased Bi:As ratio produces an elongation of the a and b lattice periods, and a shortening of the c period, and increases the frequency of twinning in kirkiite.

KW - Faculty of Science

KW - Kirkiite

KW - krystal strukturer

KW - sulfosalte

KW - kirkiite

KW - Vulcano fumaroles

KW - twinning

KW - crystal structure

KW - sulfosalts

U2 - 1221/2006/0018-0393

DO - 1221/2006/0018-0393

M3 - Journal article

VL - 18

SP - 393

EP - 401

JO - European Journal of Mineralogy

JF - European Journal of Mineralogy

SN - 0935-1221

IS - 3

ER -

ID: 80383