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Reppiaite, Mn5(OH)4(VO4)2, a new mineral from Val Graveglia (Northern Apennines, Italy)

Published/Copyright: August 24, 2010

Abstract

Reppiaite occurs in manganese ores at the Gambatesa Mine, near Reppia village (Val Graveglia, Italy), mainly associated with a Mn-sheet silicate and Mn – Ca-carbonates. It was found in small amounts of very minute tabular crystals, (100) flattened, grown in fracture. Reppiaite, with ideal formula Mn5(OH)4(VO4)2, crystallizes in C2/m space group with a = 9.604(2) Å, b = 9.558(2) Å, c = 5.393(1) Å and β = 98.45(1)°. The strongest lines in the X-ray powder pattern are d13[unk] = 2.68 Å and d200 = 4.76 Å. It is orange-red in colour, transparent, biaxial negative with 2 V large and slightly pleochroic. Microprobe analyses reveal a partial As substitution for V, leading to the empirical formula Mn5.01(OH)3.98[(V1.65-As0.35)O8.02]. The crystal structure of reppiaite is constructed of a quasi cubic close-packing of oxygens and hydroxyl groups, whose layers are stacked parallel to (100). The structure, refined to R = 0.038, consists of Mn octahedral layers bound together by isolated (V, As) tetrahedra and hydrogen bonds. Among the minerals, whose chemical formula has the same atomic proportions of reppiaite, only cornubite shows very similar structural features.

Published Online: 2010-8-24
Published in Print: 1992-2-1

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