Standard

Vendidaite, AL2(SO4)(OH)3CL·6H2O, a new mineral from La Vendida copper mine, Antofagasta region, Chile. / Chukanov, Nikita V.; Krivovichev, Sergey V.; Chernyatieva, Anastasiya P.; Möhn, Gerhard; Pekov, Igor V.; Belakovskiy, Dmitriy I.; Van, Konstantin V.; Lorenz, Joachim A.

In: Canadian Mineralogist, Vol. 51, 2013, p. 559-568.

Research output: Contribution to journal › Article

Harvard

Chukanov, NV, Krivovichev, SV, Chernyatieva, AP, Möhn, G, Pekov, IV, Belakovskiy, DI, Van, KV & Lorenz, JA 2013, 'Vendidaite, AL2(SO4)(OH)3CL·6H2O, a new mineral from La Vendida copper mine, Antofagasta region, Chile', Canadian Mineralogist, vol. 51, pp. 559-568. <http://canmin.geoscienceworld.org/content/51/4/559.short?rss=1>

APA

Chukanov, N. V., Krivovichev, S. V., Chernyatieva, A. P., Möhn, G., Pekov, I. V., Belakovskiy, D. I., Van, K. V., & Lorenz, J. A. (2013). Vendidaite, AL2(SO4)(OH)3CL·6H2O, a new mineral from La Vendida copper mine, Antofagasta region, Chile. Canadian Mineralogist, 51, 559-568. http://canmin.geoscienceworld.org/content/51/4/559.short?rss=1

Vancouver

Chukanov NV, Krivovichev SV, Chernyatieva AP, Möhn G, Pekov IV, Belakovskiy DI et al. Vendidaite, AL2(SO4)(OH)3CL·6H2O, a new mineral from La Vendida copper mine, Antofagasta region, Chile. Canadian Mineralogist. 2013;51:559-568.

Author

Chukanov, Nikita V. ; Krivovichev, Sergey V. ; Chernyatieva, Anastasiya P. ; Möhn, Gerhard ; Pekov, Igor V. ; Belakovskiy, Dmitriy I. ; Van, Konstantin V. ; Lorenz, Joachim A. / Vendidaite, AL2(SO4)(OH)3CL·6H2O, a new mineral from La Vendida copper mine, Antofagasta region, Chile. In: Canadian Mineralogist. 2013 ; Vol. 51. pp. 559-568.

BibTeX

@article{7a4fd79523574fdf9aa33b4b74f477c8,
title = "Vendidaite, AL2(SO4)(OH)3CL·6H2O, a new mineral from La Vendida copper mine, Antofagasta region, Chile",
abstract = "The new mineral vendidaite was discovered in the abandoned La Vendida mine, near Sierra Gorda, Antofagasta Region, Atacama desert, Chile. Associated minerals are aubertite, magnesioaubertite, belloite, eriochalcite, alunite, kaolinite, and halloysite. Vendidaite forms colorless platy crystals up to 0.01 × 0.3 × 0.3 mm in size; these occur in clusters up to 0.5 mm across. Vendidaite is brittle, with estimated Mohs{\textquoteright} hardness of 2–2½ and perfect cleavage on (010). Dmeas = 1.97(1) g/cm3, Dcalc = 1.974 g/cm3. The new mineral is optically biaxial (+), α = 1.522(2), β = 1.524(2), γ = 1.527(2), 2V (meas.) = 75(15)°, 2V (calc.) = 79°. Infra-red spectrum is given. The chemical composition (electron microprobe, H2O by gas chromatography) is (in wt.%): Al2O3 28.51, Fe2O3 1.39, SO3 22.38, Cl 9.87, H2O 38.8, O = Cl −2.23, total 98.72. The empirical formula is: Al1.96Fe3+0.06(SO4)0.98 Cl0.98(OH)3.12 5.98H2O. The crystal structure was solved using single-crystal X-ray diffraction data (R1 = 0.044). Vendidaite is monoclinic,",
author = "Chukanov, {Nikita V.} and Krivovichev, {Sergey V.} and Chernyatieva, {Anastasiya P.} and Gerhard M{\"o}hn and Pekov, {Igor V.} and Belakovskiy, {Dmitriy I.} and Van, {Konstantin V.} and Lorenz, {Joachim A.}",
year = "2013",
language = "не определен",
volume = "51",
pages = "559--568",
journal = "Canadian Mineralogist",
issn = "0008-4476",
publisher = "Mineralogical Association of Canada",

}

RIS

TY - JOUR

T1 - Vendidaite, AL2(SO4)(OH)3CL·6H2O, a new mineral from La Vendida copper mine, Antofagasta region, Chile

AU - Chukanov, Nikita V.

AU - Krivovichev, Sergey V.

AU - Chernyatieva, Anastasiya P.

AU - Möhn, Gerhard

AU - Pekov, Igor V.

AU - Belakovskiy, Dmitriy I.

AU - Van, Konstantin V.

AU - Lorenz, Joachim A.

PY - 2013

Y1 - 2013

N2 - The new mineral vendidaite was discovered in the abandoned La Vendida mine, near Sierra Gorda, Antofagasta Region, Atacama desert, Chile. Associated minerals are aubertite, magnesioaubertite, belloite, eriochalcite, alunite, kaolinite, and halloysite. Vendidaite forms colorless platy crystals up to 0.01 × 0.3 × 0.3 mm in size; these occur in clusters up to 0.5 mm across. Vendidaite is brittle, with estimated Mohs’ hardness of 2–2½ and perfect cleavage on (010). Dmeas = 1.97(1) g/cm3, Dcalc = 1.974 g/cm3. The new mineral is optically biaxial (+), α = 1.522(2), β = 1.524(2), γ = 1.527(2), 2V (meas.) = 75(15)°, 2V (calc.) = 79°. Infra-red spectrum is given. The chemical composition (electron microprobe, H2O by gas chromatography) is (in wt.%): Al2O3 28.51, Fe2O3 1.39, SO3 22.38, Cl 9.87, H2O 38.8, O = Cl −2.23, total 98.72. The empirical formula is: Al1.96Fe3+0.06(SO4)0.98 Cl0.98(OH)3.12 5.98H2O. The crystal structure was solved using single-crystal X-ray diffraction data (R1 = 0.044). Vendidaite is monoclinic,

AB - The new mineral vendidaite was discovered in the abandoned La Vendida mine, near Sierra Gorda, Antofagasta Region, Atacama desert, Chile. Associated minerals are aubertite, magnesioaubertite, belloite, eriochalcite, alunite, kaolinite, and halloysite. Vendidaite forms colorless platy crystals up to 0.01 × 0.3 × 0.3 mm in size; these occur in clusters up to 0.5 mm across. Vendidaite is brittle, with estimated Mohs’ hardness of 2–2½ and perfect cleavage on (010). Dmeas = 1.97(1) g/cm3, Dcalc = 1.974 g/cm3. The new mineral is optically biaxial (+), α = 1.522(2), β = 1.524(2), γ = 1.527(2), 2V (meas.) = 75(15)°, 2V (calc.) = 79°. Infra-red spectrum is given. The chemical composition (electron microprobe, H2O by gas chromatography) is (in wt.%): Al2O3 28.51, Fe2O3 1.39, SO3 22.38, Cl 9.87, H2O 38.8, O = Cl −2.23, total 98.72. The empirical formula is: Al1.96Fe3+0.06(SO4)0.98 Cl0.98(OH)3.12 5.98H2O. The crystal structure was solved using single-crystal X-ray diffraction data (R1 = 0.044). Vendidaite is monoclinic,

M3 - статья

VL - 51

SP - 559

EP - 568

JO - Canadian Mineralogist

JF - Canadian Mineralogist

SN - 0008-4476

ER -

ID: 5679693