Crystal structure of eveslogite revealed by electron diffraction techniques: a titanosilicate mineral with structurally and compositionally distinct nanoscopic tubular units

Buchsteiner, E.; Klementová, M.; Depmeier, W.; Krivovichev, S.V.; Czank, M.; Schowalter, M.; Palatinus, L.; Rozhdestvenskaya, I.V.; Yakovenchuk, V.; Kolb, U.

doi:10.1107/S2052520626008620

Figure 1
(a) A fibrous aggregate of mineral Evl from a monomineral vein in gneissose rischorrites of Eveslogchorr mountain. The length of the sample is 10 cm. Data from two untwinned crystals (b and f) were combined for the structure solution to increase the data completeness. Images of crystals and the sections through the diffraction data are shown: (b) crystal 1, (c) 0kl section, (d) h0l section, (e) hk0 section, (f) crystal 2, (g) 0kl section, (h) h0l section, (i) hk0 section. The grid of the unit cell is indicated in yellow.

STRUCTURAL SCIENCE
CRYSTAL ENGINEERING
MATERIALS

ISSN: 2052-5206

Volume 82| Part 5| October 2026| Pages 500-512

https://doi.org/10.1107/S2052520626008620

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