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metavoltine

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A structural fragment of szmolnokite (а), claster (FeO6)3O(SO4)6 (b) in the structure of metavoltine, isolated hydrated octahedra (Fe+2(H2O)6) among the metavoltine clusters within its own structure (c).
Published: 01 December 2024
Fig. 9. A structural fragment of szmolnokite ( а ), claster (FeO 6 ) 3 O(SO 4 ) 6 ( b ) in the structure of metavoltine, isolated hydrated octahedra (Fe +2 (H 2 O) 6 ) among the metavoltine clusters within its own structure ( c ).
Image
Atomic arrangements of carlsonite and metavoltine, viewed down [100]. Fe3+O6 octahedra are orange, Fe2+O6 octahedra are green, SO4 tetrahedra are yellow, K atoms are light blue spheres, Na atoms are dark blue spheres, N atoms are red spheres, O atoms of isolated H2O groups are large white spheres, and H atoms are small white spheres. N-H and O-H bonds are shown as sticks. Unit cells are shown with dashed lines.
Published: 01 September 2016
Figure 12 Atomic arrangements of carlsonite and metavoltine, viewed down [100]. Fe 3+ O 6 octahedra are orange, Fe 2+ O 6 octahedra are green, SO 4 tetrahedra are yellow, K atoms are light blue spheres, Na atoms are dark blue spheres, N atoms are red spheres, O atoms of isolated H 2 O groups
Journal Article
Published: 01 September 2016
American Mineralogist (2016) 101 (9): 2095–2107.
...Figure 12 Atomic arrangements of carlsonite and metavoltine, viewed down [100]. Fe 3+ O 6 octahedra are orange, Fe 2+ O 6 octahedra are green, SO 4 tetrahedra are yellow, K atoms are light blue spheres, Na atoms are dark blue spheres, N atoms are red spheres, O atoms of isolated H 2 O groups...
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Journal Article
Published: 01 December 2024
Russ. Geol. Geophys. (2024) 65 (12): 1468–1484.
...Fig. 9. A structural fragment of szmolnokite ( а ), claster (FeO 6 ) 3 O(SO 4 ) 6 ( b ) in the structure of metavoltine, isolated hydrated octahedra (Fe +2 (H 2 O) 6 ) among the metavoltine clusters within its own structure ( c ). ...
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Selected clusters from sulfate structures; (a) creedite; (b) minasragrite; (c) bloedite; (d) roemerite; (e) ungemachite; (f) rozenite; (g) coquimbite; (h) metavoltine. Salmon pink = (Sφ4); yellow = (Mφ6) (M = tetra-, tri- or di-valent cation).
Published: 01 August 2014
F ig . 28. Selected clusters from sulfate structures; ( a ) creedite; ( b ) minasragrite; ( c ) bloedite; ( d ) roemerite; ( e ) ungemachite; ( f ) rozenite; ( g ) coquimbite; ( h ) metavoltine. Salmon pink = (Sφ 4 ); yellow = ( M φ 6 ) ( M = tetra-, tri- or di-valent cation).
Journal Article
Published: 19 April 2023
Mineralogical Magazine (2023) 87 (5): 767–772.
... of light green–yellow equant crystals in a secondary assemblage with bobcookite, coquimbite, halotrichite, metavoltine, rhomboclase, römerite, tamarugite, voltaite and zincorietveldite. The streak is very pale green yellow and the fluorescence is strong green under 405 nm ultraviolet light. Crystals...
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Journal Article
Published: 03 March 2023
Mineralogical Magazine (2023) 87 (4): 528–533.
... with bobcookite, coquimbite, halotrichite, libbyite, metavoltine, rhomboclase, römerite, tamarugite and voltaite. The streak is very pale yellow. Crystals are transparent with vitreous lustre. The tenacity is brittle, the Mohs hardness is ~2½ and the fracture is curved. Cleavage is excellent on {010}, good...
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(a) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between ~0.31 and 0.74 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: yavapaiite (Graeber and Rosenzweig 1971), krausite (Graeber et al. 1965), goldichite (Graeber and Rosenzweig 1971), copiapite, ferricopiapite, and zincocopiapite (Fanfani et al. 1973). O atoms are shown in red, OH in gray, and Fe in orange. (b) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between 0.58 and 0.79 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: apjohnite (Menchetti and Sabelli 1976), dietrichite (Ballirano et al. 2003), metavoltine (Giacovazzo et al. 1976), starkeyite (Baur 1962), and ilesite (Held and Bohaty 2002). No crystal structure is available for bilinite. O atoms are shown in red, OH in gray, H in pink, Mg in yellow, Al in blue, and Fe in orange. Metavoltine G2677 has a römerite impurity (large QS doublet); its Fe3+ feature is nearly a singlet, as also seen in bilinite. (Color online.)
Published: 01 November 2013
. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: apjohnite ( Menchetti and Sabelli 1976 ), dietrichite ( Ballirano et al. 2003 ), metavoltine ( Giacovazzo et al. 1976 ), starkeyite ( Baur 1962 ), and ilesite ( Held and Bohaty 2002
Journal Article
Published: 08 September 2022
Mineralogical Magazine (2023) 87 (1): 151–159.
... mineral occurring with alum-(K), halotrichite, metavoltine, quartz, römerite, stanleyite, sulphur, szomolnokite and mathesiusite. It forms rectangular blades flattened on {010} and elongated on [001], reaching ~0.3 mm in length. Crystals are yellow in colour, transparent with a vitreous lustre; the streak...
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Journal Article
Published: 01 January 2021
American Mineralogist (2021) 106 (1): 105–111.
.... It is a secondary phase found on gypsum in association with copiapite, ferrinatrite, ivsite, metavoltine, and römerite. Seaborgite occurs in sprays of light-yellow, long flattened prisms or blades, up to about 0.2 mm in length. Crystals are elongated on [100], flattened on {010}, and exhibit the forms {100}, {010...
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Journal Article
Published: 17 March 2020
Mineralogical Magazine (2020) 84 (3): 435–443.
... in a secondary assemblage with belakovskiite, blödite, changoite, ferrinatrite, gypsum, ivsite, metavoltine and tamarugite. The streak is very pale yellow and the fluorescence is bright lime green under 405 nm ultraviolet light. Crystals are transparent with vitreous lustre. The tenacity is brittle, the Mohs...
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Journal Article
Published: 03 June 2019
Mineralogical Magazine (2019) 83 (6): 799–808.
... in a secondary assemblage with belakovskiite, ferrinatrite, halite, ivsite, metavoltine and thénardite. The streak is white and the fluorescence is bright cyan under 365 nm ultraviolet light. Crystals are transparent with vitreous lustre. The tenacity is brittle, the Mohs hardness is 2½, the fracture...
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Journal Article
Published: 01 July 2018
European Journal of Mineralogy (2018) 30 (4): 801–809.
... Loa province, Antofagasta region, Chile. It is associated with römerite, coquimbite, metavoltine, tamarugite, halotrichite, szomolnokite, rhomboclase, and ferricopiapite. Calamaite forms acicular to hair-like crystals up to 0.01 × 2 mm combined in bunches or radial spherulitic clusters up to 4 mm...
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Journal Article
Published: 01 June 2014
Mineralogical Magazine (2014) 78 (3): 639–649.
... in association with blödite, ferrinatrite, kröhnkite, meisserite and metavoltine. Crystals of belakovskiite are very pale yellowish-green hair-like fibres up to 2 mm long and usually no more than a few μm in diameter. The fibres are elongated on [100] and slightly flattened on {021}. Crystals are transparent...
FIGURES
Journal Article
Published: 01 February 2012
The Canadian Mineralogist (2012) 50 (1): 65–72.
..., and hexahydrite, but other ammonium minerals (salammoniac, mascagnite, clairite, boussingaultite, efremovite, koktaite, mohrite, ammoniojarosite, godovikovite, letovicite) as well as native sulfur, millosevichite, alunogen, metavoltine, voltaite, gypsum, anhydrite, halotrichite, butlerite, jarosite, and copiapite...
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Journal Article
Published: 01 December 2010
The Canadian Mineralogist (2010) 48 (6): 1465–1468.
..., Italy. It occurs as colorless to pale pink tabular or short prismatic crystals up to 0.5 mm in size in association with alunogen, coquimbite, krausite, tamarugite, voltaite, pertlikite, yavapaiite, pickeringite and metavoltine. The mineral is trigonal, space group P 3̅1 c (no. 163), with a 10.7065(7), c...
FIGURES
Journal Article
Published: 01 June 2008
The Canadian Mineralogist (2008) 46 (3): 661–669.
..., Iran, the mineral occurs in a pyrite-bearing trachytic eruptive rock, and probably formed after the decomposition of pyrite. Pertlikite forms single crystals up to 1 cm; the phase is associated with metavoltine, botryogen, pyrite and alunite. In contrast to voltaite and zincovoltaite, the optical...
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Journal Article
Published: 01 June 2008
The Canadian Mineralogist (2008) 46 (3): 693–700.
..., Sicily, Italy. The mineral occurs as sharp translucent crystals up to 0.25 mm in an altered pyroclastic breccia, together with alunite, sassolite, anhydrite and metavoltine. It is orthorhombic ( mmm ), space group Pbcn , with a 10.810(2), b 8.336(2), c 6.822(1) Å, V 614.8(2) Å 3 , Z = 4; the crystal...
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Image
(a) The structure of quenstedtite; (b) the arrangement of [Mg(SO4)4(H2O)2] clusters in polyhalite; (c) polyhalite as a framework of (MgØ6) octahedra, (CaØ8) polyhedra, and (SO4) tetrahedra; (d) thestructure of rozenite; (e) the sheet of [Fe3+(SO4)6] clusters, (NO3) groups, and K atoms in ungemachite; (f) the arrangement of columns and their linkage through hydrogen bonding in ungemachite. (g) The structure of coquimbite, and (h) the structure of metavoltine.
Published: 01 January 2000
) groups, and K atoms in ungemachite; (f) the arrangement of columns and their linkage through hydrogen bonding in ungemachite. (g) The structure of coquimbite, and (h) the structure of metavoltine.
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(a) The structure of quenstedtite; (b) the arrangement of [Mg(SO4)4(H2O)2] clusters in polyhalite; (c) polyhalite as a framework of (MgØ6) octahedra, (CaØ8) polyhedra, and (SO4) tetrahedra; (d) thestructure of rozenite; (e) the sheet of [Fe3+(SO4)6] clusters, (NO3) groups, and K atoms in ungemachite; (f) the arrangement of columns and their linkage through hydrogen bonding in ungemachite. (g) The structure of coquimbite, and (h) the structure of metavoltine.
Published: 01 January 2000
) groups, and K atoms in ungemachite; (f) the arrangement of columns and their linkage through hydrogen bonding in ungemachite. (g) The structure of coquimbite, and (h) the structure of metavoltine.