2007 ÇÀÏÈÑÊÈ ÐÎÑÑÈÉÑÊÎÃÎ ÌÈÍÅÐÀËÎÃÈ×ÅÑÊÎÃÎ ÎÁÙÅÑÒÂÀ ×. CXXXVI, ¹ 4 2007 ZAPISKI RMO (PROCEEDINGS OFTHE RUSSIAN MINERALOGICAL SOCIETY) Pt CXXXVI, N 4 ÍÎÂÛÅ ÌÈÍÅÐÀËÛ ÓÄÊ 549.6 © Ïî÷åòíûé ÷ë. À. Ï. ÕÎÌßÊÎÂ,* ä. ÷ë. Ã. Í. ÍÅ×ÅËÞÑÒÎÂ,** ä. ÷ë. Ð. Ê. ÐÀÑÖÂÅÒÀÅÂÀ*** ÄÓÀËÈÒ Na30(Ca,Na,Ce,Sr)12(Na,Mn,Fe,Ti)6Zr3Ti3MnSi51O144(OH,H2O,Cl)9 — ÍÎÂÛÉ ÖÈÐÊÎÍÎ-ÒÈÒÀÍÎÑÈËÈÊÀÒ Ñ ÌÎÄÓËßÐÍÎÉ ÝÂÄÈÀËÈÒÎÏÎÄÎÁÍÎÉ ÑÒÐÓÊÒÓÐÎÉ ÈÇ ËÎÂÎÇÅÐÑÊÎÃÎ ÙÅËÎ×ÍÎÃÎ ÌÀÑÑÈÂÀ, ÊÎËÜÑÊÈÉ ÏÎËÓÎÑÒÐÎÂ, ÐÎÑÑÈß1 A. P. KHOMYAKOV, G. N. NECHELYUSTOV, R. K. RASTSVETAEVA. DUALITE, Na30(Ca,Na,Ce,Sr)12(Na,Mn,Fe,Ti)6Zr3Ti3MnSi51O144(OH,H2O,Cl)9, A NEW ZIRCONO-TITANOSILICATE WITH A MODULAR EUDIALYTE-LIKE STRUCTURE FROM LOVOZERO ALKALINE MASSIF, KOLA PENINSULA, RUSSIA * Èíñòèòóò ìèíåðàëîãèè, ãåîõèìèè è êðèñòàëëîõèìèè ðåäêèõ ýëåìåíòîâ, 121357, Ìîñêâà, óë. Âåðåñàåâà, 15; e-mail:
[email protected] ** Âñåðîññèéñêèé íàó÷íî-èññëåäîâàòåëüñêèé èíñòèòóò ìèíåðàëüíîãî ñûðüÿ, 109017, Ìîñêâà, Ñòàðîìîíåòíûé ïåð., 31 *** Èíñòèòóò êðèñòàëëîãðàôèè ÐÀÍ, 117333, Ìîñêâà, Ëåíèíñêèé ïð., 59 Dualite was found on Mt. Alluaiv (Lovozero massif, Kola Peninsula), in hyperagpaitic pegmatoid rock as rare anhedral grains up to 0.3—0.5 mm across. Associated minerals are: sodium-potassium feldspar, nepheline, sodali- te, cancrinite, aegirine, alkaline amphibole, eudialyte, lovozerite, lomonosovite, vuonnemite, lamprophyllite, spha- lerite and villiaumite. It is yellow, transparent or translucent, with conchoidal fracture; brittle; luster vitreous; streak white. Mohs’ hardness 5. D(meas.) = 2.84(3) g/cm3 (volumetric method), D(calc.) = 2.814 g/cm3. The mineral dis- solves and gelatinises in acid at room temperature. Non-fluorescent. Optically uniaxial, positive, no = 1.610(1), 3 ne = 1.613(1). Trigonal, space group R3m, a = 14.153(9), c = 60.72(5) Å, V = 10533(22) Å , Z = 3.