Abstract
The crystal structure of a Ta-free Nb-dominant ixiolite analogue with the empirical formula (Nb1.55Ti1.11\({\text{Fe}}_{{1.01}}^{{3 + }}{\text{Mn}}_{{0.19}}^{{2 + }}{\text{Cr}}_{{0.04}}^{{3 + }}\)Mg0.04Al0.03Zr0.02\({\text{Mn}}_{{0.01}}^{{3 + }}\))Σ4O8 (Z = 1) from the Laach Lake area (Eifel, Germany) has been studied on the basis of single-crystal X-ray diffraction data and refined in the space group Pbcn to R = 4.47%. The unit-cell parameters are a = 4.6578(6), b = 5.6230(7), c = 5.0182(5) Å, and V = 131.43(3) Å3. The mineral belongs to the α-PbO2 structure type. It was found in volcanic nosean sanidinite, in a late (presumably, pneumatolytic) mineral assemblage containing sanidine, nosean, magnetite, ilmenite, biotite, corundum, and columbite-(Fe). The crystal chemistry of the ixiolite-like niobate has been discussed, including an aspect related to the definition of the discredited mineral species “ashanite.”
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Funding
This work was supported by the Russian Science Foundation (grant no. 19-17-00050; structural research, crystallochemical and mineralogenetic analysis). The chemical composition of the mineral was studied in the framework of a state assignment, state registration no. АALA-А19-119092390076-7.
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Translated by E. Maslennikova
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Zubkova, N.V., Chukanov, N.V., Pekov, I.V. et al. Ta-Free Nb-Dominant Ixiolite Analogue from the Eifel Paleovolcanic Region, Germany, and Its Crystal Structure. On the Problem of “Ashanite”. Geol. Ore Deposits 63, 805–811 (2021). https://doi.org/10.1134/S1075701521080110
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DOI: https://doi.org/10.1134/S1075701521080110