Filatovite, K[(Al,Zn)2(As,Si)2O8], a new mineral species from the Tolbachik volcano, Kamchatka peninsula, Russia

被引:26
|
作者
Vergasova, LP
Krivovichev, SV
Britvin, SN
Burns, PC
Ananiev, VV
机构
[1] St Petersburg State Univ, Dept Crystallog, St Petersburg 199034, Russia
[2] Russian Acad Sci, Inst Volcanol, Petropavlovsk Kamchatski 683006, Russia
[3] Univ Kiel, Inst Geowissensch Mineral Kristallog, D-24118 Kiel, Germany
[4] St Petersburg State Univ, Dept Mineral Deposits, St Petersburg 199034, Russia
[5] Univ Notre Dame, Dept Civil Engn & Geol Sci, Notre Dame, IN 46556 USA
关键词
filatovite; arsenic; feldspar group; Tolbachik volcano; Russia;
D O I
10.1127/0935-1221/2004/0016-0533
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
Filatovite, ideally K[(Al,Zn)(2)(As,Si)(2)O-8], has been found in products of fumarolic activity on the second cinder cone of the North breach of the great fissure Tolbachik eruption (1975-76, Kamchatka peninsula, Russia). The mineral occurs as prismatic crystals up to 0.3 mm and as intergrowths of crystals, in association with alumoklyuchevskite, lammerite, johillerite, sylvite, As-bearing orthoclase, hematite and tenorite. Filatovite is colourless, with vitreous luster and white streak. The mineral is brittle and transparent. It has a good 11001 cleavage. Mohs' hardness is 5-6. The calculated density is 2.92 g/cm(3). Biaxial, optically negative alpha = 1.532(1), beta = 1.535(1), gamma = 1.537(1), 2V(meas.) = 60(10)degrees, 2V(calc.) = 78degrees. Optical orientation: X similar to [100], Y and Z are normal to the {001} and {010} faces, respectively. No pleochroism has been observed. The mineral is monoclinic, space group I2/c, a = 8.772(1), b = 13.370(2), c = 14.690(2) Angstrom, beta = 115.944(6)degrees, V = 1549.1(4) Angstrom(3), Z = 8 (from single-crystal structure study). The diagnostic lines of the X-ray powder diffraction pattern are (I-d-hkl): 70-4.329-(2) over bar 02; 70-3.897-130; 100-3.364-(2) over bar 20, (2) over bar 04, 040; 50-3.300-004, 40-3.066-132, 60-2.981-042, 40-2.646-(2) over tilde 42. Chemical composition (wt. %): P2O5 1.63, As2O5 40.60, SiO2 12.35, Al2O3 27.33, CuO 0.83, ZnO 3.85, FeO 0.28, Na2O 0.63, K2O 12.85, total 100.35. The empirical formula of filatovite, calculated on the basis of O = 8, is (K0.92Na0.07)(Sigma=0.99)[(Al1.81Zn0.16Cu0.04Fe0.01)(Sigma=2.02)(As1.20Si0.70P0.08)(Sigma=1.98)O-8]. The simplified formula is K[(Al,Zn)(2)(As,Si)(2)O-8]. The detailed chemical formula can be written as K[(Al2-xZnx)(As1+xSi1-x)O-8], with x similar to 0.20. Filatovite is a new mineral of the feldspar group and is structurally related to celsian. The name honors Prof. Stanislav K. Filatov (b. 1940), Department of Crystallography, St. Petersburg State University, St. Petersburg, Russia, for his important contributions to high temperature crystal chemistry and crystal chemistry of exhalation minerals.
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页码:533 / 536
页数:4
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