Инд. авторы:	Sharygin V.V., Doroshkevich A.G., Seryotkin Y.V., Karmanov N.S., Moroz T.N., Nigmatulina E.N., Yelisseyev A.P., Vedenyapin V.N., Kupriyanov I.N., Belogub E.V.
Заглавие:	Rippite, k2nb2(si4o12)o2)o(o,f), a new k-nb-cyclosilicate from chuktukon carbonatite massif, chadobets upland, krasnoyarsk territory, russia
Библ. ссылка:	Sharygin V.V., Doroshkevich A.G., Seryotkin Y.V., Karmanov N.S., Moroz T.N., Nigmatulina E.N., Yelisseyev A.P., Vedenyapin V.N., Kupriyanov I.N., Belogub E.V. Rippite, k2nb2(si4o12)o2)o(o,f), a new k-nb-cyclosilicate from chuktukon carbonatite massif, chadobets upland, krasnoyarsk territory, russia // Minerals. - 2020. - Vol.10. - Iss. 12. - P.1-28. - EISSN 2075-163X.
Внешние системы:	DOI: 10.3390/min10121102; РИНЦ: 45083025;
Реферат:	eng: Rippite K2(Nb,Ti)2(Si4O12)(O,F)2, a new K-Nb-cyclosilicate, has been discovered in calciocarbonatites from the Chuktukon massif (Chadobets upland, SW Siberian Platform, Krasnoyarsk Territory, Russia). It was found in a primary mineral assemblage, which also includes calcite, fluorcalciopyrochlore, tainiolite, fluorapatite, fluorite, Nb-rich rutile, olekminskite, K-feldspar, Fe-Mn–dolomite and quartz. Goethite, francolite (Sr-rich carbonate–fluorapatite) and psilomelane (romanèchite ± hollandite) aggregates as well as barite, monazite-(Ce), parisite-(Ce), synchysite-(Ce) and Sr-Ba-Pb-rich keno-/hydropyrochlore are related to a stage of metasomatic (hydrothermal) alteration of carbonatites. The calcite–dolomite coexistence assumes crystallization temperature near 837◦C for the primary carbonatite paragenesis. Rippite is tetragonal: P4bm, a = 8.73885(16), c = 8.1277(2) Å, V = 620.69(2) Å3, Z = 2. It is closely identical in the structure and cell parameters to synthetic K2Nb2(Si4O12)O2 (or KNbSi2O7). Similar to synthetic phase, the mineral has nonlinear properties. Some optical and physical properties for rippite are: colorless; Mohs’ hardness—4–5; cleavage—(001) very perfect, (100) perfect to distinct; density (meas.)—3.17(2) g/cm3; density (calc.)—3.198 g/cm3; optically uniaxial (+); ω = 1.737-1.739; ε = 1.747 (589 nm). The empirical formula of the holotype rippite (mean of 120 analyses) is K2(Nb1.90Ti0.09Zr0.01)[Si4O12](O1.78OH0.12F0.10). Majority of rippite prismatic crystals are weakly zoned and show Ti-poor composition K2(Nb1.93Ti0.05Zr0.02)[Si4O12](O1.93F0.07). Raman and IR spectroscopy, and SIMS data indicate very low H2O content (0.09–0.23 wt %). Some grains may contain an outermost zone, which is enriched in Ti (+Zr) and F, up to K2(Nb1.67Ti0.32Zr0.01)[Si4O12](O1.67F0.33). It strongly suggests the incorporation of (Ti,Zr) and F in the structure of rippite via the isomorphism Nb5+ + O2− → (Ti,Zr)4+ + F1−. The content of a hypothetical end-member K2Ti2[Si4O12]F2 may be up to 17 mol. %. Rippite represents a new structural type among [Si4O12]-cyclosilicates because of specific type of connection of the octahedral chains and [Si4O12]8− rings. In structural and chemical aspects it seems to be in close with the labuntsovite-supergroup minerals, namely with vuoriyarvite-(K), K2(Nb,Ti)2(Si4O12)(O,OH)2·4H2O.
Ключевые слова:	Synthetic K2Nb2(Si4O12)O2; rippite; new mineral; Krasnoyarsk territory; K-Nb-cyclosilicate; Chuktukon massif; Chadobets upland; Calciocarbonatite;
Издано:	2020
Физ. характеристика:	с.1-28
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