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ISSN 00125008, Doklady Chemistry, 2012, Vol. 442, Part 2, pp. 57–62. © Pleiades Publishing, Ltd., 2012. Original Russian Text © R.K. Rastsvetaeva, S.M. Aksenov, N.V. Chukanov, 2012, published in Doklady Akademii Nauk, 2012, Vol. 442, No. 6, pp. 766–770. CHEMISTRY Crystal Structure of Günterblassite, a New Mineral with a Triple Tetrahedral Layer a a b R. K. Rastsvetaeva , S. M. Aksenov , and N. V. Chukanov Presented by Academician L.N. Kogarko June 16, 2011 Received June 17, 2011 DOI: 10.1134/S0012500812020115 Postmagmatic parageneses of the Eifel volcanic microprobe analysis. The content of H O was quanti field (Germany) are characterized by a wide variety of fied by chromatographic analysis of gaseous products of calcination. The IR spectrum of the mineral shows minerals [1]. Günterblassite is a new mineral discov the absence of borate, carbonate, nitrate, and ammo ered in a late association formed in the cavities of the alkaline basalt of the Rother Kopf mountain. The nium groups. The empirical formula calculated for 13 chemical composition was determined by electron atoms (Si, Al) is 2+ Na K Ba Ca Mg Fe[( Si Al O OH)] ⋅ 7H O 0.14 1.23 0.30 0.71 0.16 0.48 8.83 3.06 24.17 4.83 2
Doklady Chemistry – Springer Journals
Published: Mar 17, 2012
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