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Hilarionite, Fe 2 3+ (SO4)(AsO4)(OH) · 6H2O, a new supergene mineral from Lavrion, Greece

Authors :
Anna G. Turchkova
D. I. Belakovsky
V. O. Yapaskurt
Nikita V. Chukanov
Igor V. Pekov
Athanasios Katerinopoulos
Panagiotis Voudouris
Andreas Magganas
Vyacheslav S. Rusakov
Source :
Geology of Ore Deposits. 56:567-575
Publication Year :
2014
Publisher :
Pleiades Publishing Ltd, 2014.

Abstract

A new mineral, hilarionite, ideally Fe 2 3+ (SO4)(AsO4)(OH) · 6H2O, has been found in the Hilarion Mine, Agios Konstantinos, Kamariza, Lavrion district, Attiki Prefecture, Greece. It was formed in the oxidation zone of a sulfide-rich orebody in association with goethite, gypsum, bukovskyite, jarosite, melanterite, chalcanthite, allophane, and azurite. Hilarionite occurs as light green (typically with an olive or grayish tint) to light yellowish green spherulites (up to 1 mm in size) and bunches of prismatic to acicular “individuals” up to 0.5 mm long that are in fact near-parallel or divergent aggregates of very thin, curved fibers up to 0.3 mm long and usually lesser than 2 μm thick. The luster is silky to vitreous. The Mohs’ hardness is ca. 2. Hilarionite is ductile, its “individuals” are flexible and inelastic; fracture is uneven or splintery. D(meas) = 2.40(5), D(calc) = 2.486 g/cm3. IR spectrum shows the presence of arsenate and sulfate groups and H2O molecules in significant amounts. The Mossbauer spectrum indicates the presence of Fe3+ at two six-fold coordinated sites and the absence of Fe2+. Hilarionite is optically biaxial (+), α = 1.575(2), γ = 1.64(2), 2V is large. The chemical composition (electron microprobe, average of 7 point analyses; H2O determined by modified Penfield method) is as follows, wt %: 0.03 MnO, 0.18 CuO, 0.17 ZnO, 33.83 Fe2O3, 0.22 P2O5, 18.92 As2O5, 22.19 SO3, 26.3 H2O, total is 101.82%. The empirical formula calculated on the basis of 15 O is: (Fe 1.90 3+ Cu0.01Zn0.01)Σ1.92[(SO4)1.24(AsO4)0.74(PO4)0.01]Σ1.99(OH)1.01 · 6.03H2O. The X-ray powder diffraction data show close structural relationship of hilarionite and kaňkite, Fe 2 3+ (AsO4)2 · 7H2O. Hilarionite is monoclinic, space group C2/m, Cm or C2, a = 18.53(4), b = 17.43(3), c = 7.56(1) A, β = 94.06(15)°, V = 2436(3) A3, Z = 8. The strongest reflections in the X-ray powder diffraction pattern (d, A-I[hkl]) are: 12.66–100[110], $$7.60 - 6[00\bar 1]$$ , 5.00–10[22l], $$4.70 - 10[31\bar 1]$$ , 4.33–7[040]. Hilarionite is named after its type locality.

Details

ISSN :
15556476 and 10757015
Volume :
56
Database :
OpenAIRE
Journal :
Geology of Ore Deposits
Accession number :
edsair.doi...........44d7c886748d6e9eea960868421ee884
Full Text :
https://doi.org/10.1134/s1075701514070101