• journal_title：European Journal of Mineralogy
• Contributor：Alf Olav Larsen ; Uwe Kolitsch ; Robert A. Gault ; Gerald Giester
• Publisher：E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
• Date：2010-
• Format：text/html
• Language：en
• Identifier：10.1127/0935-1221/2010/0022-2068
• journal_abbrev：Eur J Mineral
• issn：0935-1221
• volume：22
• issue：6
• firstpage：875
• section：Other articles

Eirikite, ideally, KNa₆[Be₂(Si₁₅Al₃)_{∑= 18}O₃₉F₂], is a new mineral species from the Vesle Arøya island in the Langesundsfjord district, Larvik, Vestfold, Norway. It is the potassium analogue of leifite, NaNa₆[Be₂(Si₁₅Al₃)_∑=18O₃₉F₂], and telyushenkoite, CsNa₆[Be₂(Si₁₅Al₃)_{∑= 18}O₃₉F₂]. An average of five electron microprobe analyses gave Na₂O 13.38, K₂O 3.13, Al₂O₃ 11.08, SiO₂ 66.03, F 2.70, BeO 3.65 (calc.), O = F −1.14, total 98.83 wt. %, resulting in the empirical formula K_0.91Na_5.92[Be₂(Si_15.07Al_2.98)_∑=18.05]O₃₉(F_1.95O_0.05); infrared spectroscopy indicates the absence of OH and H₂O.

Eirikite occurs as both finely or coarsely fibrous, monomineralic aggregates and bundles up to 3 cm across, wholly or partly filling voids between larger microcline crystals. Individual acicular-prismatic crystals show the forms {101̅0}and {0001}. Eirikite also occurs as aggregates up to 100 cm³ in volume, built of interlocking, radiating fibrous groups, each up to 5 mm across, intergrown with large amounts of small zircon crystals and penetrated by aegirine crystals. Polylithionite, albite, eudialyte, catapleiite and pyrochlore can be found within these aggregates. Eirikite is white to colourless with a white streak, a vitreous to silky lustre, Mohs hardness of 6; it is brittle with an uneven to conchoidal fracture, and with a good {101̅0} cleavage. The mineral is uniaxial positive, ω=1.517(1) and ε = 1.521(1), and nonpleochroic; D_meas = 2.59(1) g/cm³, D_calc = 2.577 g/cm³ (from the empirical chemical formula) and 2.584 g/cm³ (from the crystal structure determination).

Eirikite is trigonal, P3̅m1 (no. 164), with a = 14.3865(9) Å, c = 4.8733(4) Å, V = 873.5(1) ų, and Z = 1, refined from X-ray powder diffraction data. The five strongest lines in the X-ray powder pattern are [d (in Å) (I/I₀)(hkl)]: 4.710(29)(120), 4.153(21)(030), 3.386(70)(211), 3.161(100)(031), and 2.466(31)(231). The crystal structure, which was determined from single-crystal X-ray intensity data and refined to R1(F) = 1.99 %, is a framework of corner-sharing (Si,Al)O₄ and BeO₃F tetrahedra (<Be–(O,F)> = 1.610 Å), leading to chain and ring units. Voids in the framework are occupied by K (<K–O>= 3.105 Å), and seven-coordinated Na atoms (<Na–(O,F)> = 2.542 Å). The B site, which is vacant in telyushenkoite and partly occupied by water molecules in leifite, is nearly vacant in eirikite.