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RESEARCH PRODUCT
Ronneburgite, K2MnV4O12, a new mineral from Ronneburg, Thuringia, Germany: Description and crystal structure
Thomas WitzkeShenyan ZhenLutz NasdalaKarl SeffUwe KolitschThomas Doeringsubject
CrystalCrystallographyGeophysicsOctahedronGeochemistry and PetrologyChemistryEmpirical formulaVanadateElectron microprobeCrystal structureRefractive indexIondescription
Ronneburgite is a new chain vanadate mineral from Ronneburg, Thuringia, Germany. It occurs as reddish-brown crystals of equant, flattened, or short prismatic habit, up to 0.5 mm in length. The crystals have an adamantine luster and are translucent. Ronneburgite is biaxial negative with refractive indices n α = 1.925(5), n β = 1.960(10), n γ = 1.988(4), and 2 V x = 82°. Electron microprobe analysis (K 2 O = 16.93, MnO = 12.44, MgO = 0.62, V 2 O 5 = 68.54; total = 98.53 wt%) gives the empirical formula K 1.91 Mn 0.93 Mg 0.08 V 4.00 O 11.96 , which simplifies to K 2 MnV 4 O 12 . Ronneburgite is mono-clinic, space group P 2 1 / n , with a = 8.183(3), b = 9.247(3), c = 8.651(2) A, and β = 109.74(2)°. The measured density is 2.84 g/cm 3 ; the calculated density for Z = 2 is 2.85 g/cm 3 . Single-crystal X-ray structure determination (R 1 = 0.046 for 1846 reflections) shows that ronneburgite contains infinite vierer-single metavanadate chains [(VO 3 ) n ] n− of corner-sharing VO 4 tetrahedra along [101]. Although the empirical formula and calculated bond valences indicate that V is 5+ and Mn is 2+, the crystal color, a “poor” structural compatibility index, and Mn-O distances between those expected for Mn 2+ -O and Mn 3+ -O indicate that some Mn 3+ and V 4+ ions are present. K + ions and octahedral Mn n+ ions bridge between the metavanadate chains by coordinating to their oxygen atoms.
year | journal | country | edition | language |
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2001-09-01 | American Mineralogist |