Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
New arsenate minerals from the Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. XX. Evseevite, Na2Mg(AsO4)F, the first natural arsenate with an antiperovskite structure. / Pekov, Igor V.; Zubkova, Natalia V.; Agakhanov, Atali A.; Vigasina, Marina F.; Yapaskurt, Vasiliy O.; Britvin, Sergey N.; Turchkova, Anna G.; Sidorov, Evgeny G.; Zhitova, Elena S.; Pushcharovsky, Dmitry Yu.
в: Mineralogical Magazine, 29.06.2023, стр. 1-10.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - New arsenate minerals from the Arsenatnaya fumarole, Tolbachik volcano, Kamchatka, Russia. XX. Evseevite, Na2Mg(AsO4)F, the first natural arsenate with an antiperovskite structure
AU - Pekov, Igor V.
AU - Zubkova, Natalia V.
AU - Agakhanov, Atali A.
AU - Vigasina, Marina F.
AU - Yapaskurt, Vasiliy O.
AU - Britvin, Sergey N.
AU - Turchkova, Anna G.
AU - Sidorov, Evgeny G.
AU - Zhitova, Elena S.
AU - Pushcharovsky, Dmitry Yu.
PY - 2023/6/29
Y1 - 2023/6/29
N2 - The new mineral evseevite was found in the Arsenatnaya fumarole, Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Evseevite is represented by two chemical varieties. The variety close to the end-member Na 2 Mg(AsO 4 )F (holotype) is associated with sanidine, hematite, tenorite, aegirine, cassiterite, sylvite, halite, johillerite, badalovite, calciojohillerite, hatertite, arsmirandite, yurmarinite, axelite, polyarsite, aphthitalite, potassic-magnesio-fluoro-arfvedsonite, litidionite, ferrisanidine and tridymite. The P- and S-enriched variety (cotype) is associated with hematite, fluorophlogopite, svabite, fluorapatite, tilasite, calciojohillerite, forsterite, cassiterite, belomarinaite and aphthitalite. Evseevite occurs as prismatic, acicular or hair-like crystals up to 0.7 mm long combined in clusters up to 0.5 mm, brushes or crusts up to 2 × 2 mm. It is transparent, colourless or pale pinkish, with vitreous lustre. D calc is 3.377 g cm –3 for the holotype and 3.226 g cm –3 for the cotype. Evseevite is optically uniaxial (+), α = 1.545(2), β = 1.546(2), γ = 1.549(2) and 2V meas = 40(10)°. The empirical formulae calculated based on O+F = 5 apfu are (Na 1.99 Ca 0.03 K 0.01 ) Σ2.03 (Mg 0.98 Fe 3+ 0.01 Zn 0.01 Cu 0.01 ) Σ1.01 [(As 0.98 Si 0.01 ) Σ1.01 O 4 ](F 0.97 O 0.03 ) for the holotype and Na 2.02 (Mg 1.00 Fe 3+ 0.03 ) Σ1.03 [(As 0.69 P 0.25 S 0.07 ) Σ1.01 O 4 ](F 0.78 O 0.22 ) for the cotype. Evseevite is orthorhombic, Pbcn , a = 5.3224(1), b = 14.1255(3), c = 12.0047(3) Å, V = 902.53(4) Å 3 and Z = 8. Strong reflections of the powder XRD pattern [ d ,Å( I )( hkl )] are: 4.001(100)(121), 3.479(56)(023), 3.041(45)(042), 2.657(44)(200), 2.642(68)(142) and 2.613(36)(104). The crystal structure was solved from single-crystal XRD data and refined on powder data by the Rietveld method, R wp = 0.0068, R p = 0.0047 and R obs = 0.0435. Evseevite is isostructural to moraskoite Na 2 Mg(PO 4 )F. The structure of evseevite can be described in terms of anion-centred polyhedra. F-centred octahedra [FNa 4 Mg 2 ] 7+ share faces to form chains [FNa 2 Mg] 3+ and AsO 4 tetrahedra are located between the chains. Evseevite belongs to a small set of minerals with antiperovskite structures and is the first natural arsenate with antiperovskite units. The mineral is named in honour of the Russian mineralogist Aleksandr Andreevich Evseev (born 1949).
AB - The new mineral evseevite was found in the Arsenatnaya fumarole, Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia. Evseevite is represented by two chemical varieties. The variety close to the end-member Na 2 Mg(AsO 4 )F (holotype) is associated with sanidine, hematite, tenorite, aegirine, cassiterite, sylvite, halite, johillerite, badalovite, calciojohillerite, hatertite, arsmirandite, yurmarinite, axelite, polyarsite, aphthitalite, potassic-magnesio-fluoro-arfvedsonite, litidionite, ferrisanidine and tridymite. The P- and S-enriched variety (cotype) is associated with hematite, fluorophlogopite, svabite, fluorapatite, tilasite, calciojohillerite, forsterite, cassiterite, belomarinaite and aphthitalite. Evseevite occurs as prismatic, acicular or hair-like crystals up to 0.7 mm long combined in clusters up to 0.5 mm, brushes or crusts up to 2 × 2 mm. It is transparent, colourless or pale pinkish, with vitreous lustre. D calc is 3.377 g cm –3 for the holotype and 3.226 g cm –3 for the cotype. Evseevite is optically uniaxial (+), α = 1.545(2), β = 1.546(2), γ = 1.549(2) and 2V meas = 40(10)°. The empirical formulae calculated based on O+F = 5 apfu are (Na 1.99 Ca 0.03 K 0.01 ) Σ2.03 (Mg 0.98 Fe 3+ 0.01 Zn 0.01 Cu 0.01 ) Σ1.01 [(As 0.98 Si 0.01 ) Σ1.01 O 4 ](F 0.97 O 0.03 ) for the holotype and Na 2.02 (Mg 1.00 Fe 3+ 0.03 ) Σ1.03 [(As 0.69 P 0.25 S 0.07 ) Σ1.01 O 4 ](F 0.78 O 0.22 ) for the cotype. Evseevite is orthorhombic, Pbcn , a = 5.3224(1), b = 14.1255(3), c = 12.0047(3) Å, V = 902.53(4) Å 3 and Z = 8. Strong reflections of the powder XRD pattern [ d ,Å( I )( hkl )] are: 4.001(100)(121), 3.479(56)(023), 3.041(45)(042), 2.657(44)(200), 2.642(68)(142) and 2.613(36)(104). The crystal structure was solved from single-crystal XRD data and refined on powder data by the Rietveld method, R wp = 0.0068, R p = 0.0047 and R obs = 0.0435. Evseevite is isostructural to moraskoite Na 2 Mg(PO 4 )F. The structure of evseevite can be described in terms of anion-centred polyhedra. F-centred octahedra [FNa 4 Mg 2 ] 7+ share faces to form chains [FNa 2 Mg] 3+ and AsO 4 tetrahedra are located between the chains. Evseevite belongs to a small set of minerals with antiperovskite structures and is the first natural arsenate with antiperovskite units. The mineral is named in honour of the Russian mineralogist Aleksandr Andreevich Evseev (born 1949).
UR - https://www.mendeley.com/catalogue/823a154d-db84-36f4-93b0-5277565016e5/
U2 - 10.1180/mgm.2023.50
DO - 10.1180/mgm.2023.50
M3 - Article
SP - 1
EP - 10
JO - Mineralogical Magazine
JF - Mineralogical Magazine
SN - 0026-461X
ER -
ID: 108742508