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G. Ferraris, A. Gula (2005)
Polysomatic aspects of microporous minerals - heterophyllosilicates, palysepioles and rhodesite-related structuresReviews in Mineralogy & Geochemistry, 57
R. Rastsvetaeva, I. Ekimenkova, I. Pekov (1999)
CRYSTAL STRUCTURE OF A NEW HIGH-CALCIUM ANALOGUE OF EUDIALYTEDoklady Chemistry, 368
N. Walker, D. Stuart (1983)
An empirical method for correcting diffractometer data for absorption effectsActa Crystallographica Section A, 39
ISSN 00125008, Doklady Chemistry, 2011, Vol. 437, Part 2, pp. 90–94. © Pleiades Publishing, Ltd., 2011. Original Russian Text © R.K. Rastsvetaeva, S.M. Aksenov, N.V. Chukanov, 2011, published in Doklady Akademii Nauk, 2011, Vol. 437, No. 4, pp. 499–503. CHEMISTRY Crystal Structure of Schüllerite, a New Mineral of the Heterophyllosilicate Family a a b R. K. Rastsvetaeva , S. M. Aksenov , and N. V. Chukanov Presented by Academician L.N. Kogarko October 8, 2010 Received October 19, 2010 DOI: 10.1134/S0012500811040045 The representative family of heterophyllosilicates Triclinic cell parameters: a = 5.4027(1), b = includes, in particular, the lamprophyllite group. The 7.066(4), c = 10.2178(1) Å, α = 99.816(1)°, β = structure of the lamprophyllite group minerals is based 99.624(1)°, γ = 90.084(1)°; space group P1. The crys on threelayer blocks composed of the cationic wall tal data and Xray experiment details are summarized made of edgesharing octahedra and the anionic net in Table 1. All calculations were carried out using the work of Si diortho groups combined by Ti semioctahe AREN program package [3, 4]. dra. The anionic networks are attached to the octahe The structure of the cationic fragment was deter dral layer through the vertices of the
Doklady Chemistry – Springer Journals
Published: May 12, 2011
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