Ultrahigh potassium content in the clinopyroxene structure: an X-ray single-crystal study

被引:16
作者
Bindi, L
Safonov, OG
Litvin, YA
Perchuk, LL
Menchetti, S
机构
[1] Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy
[2] Inst Expt Mineral, Chernogolovka 142432, Moscow District, Russia
[3] Moscow MV Lomonosov State Univ, Dept Geol, Moscow 119899, Russia
关键词
potassium-bearing clinopyroxene; structure refinement; single-crystal X-ray diffraction; synthetic crystals; chemical analysis;
D O I
10.1127/0935-1221/2002/0014-0929
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The crystal structures and chemical compositions of two crystals of clinopyroxene (labelled K1 and K2) synthesized in the model system CaMgSi2O6 - KAlSi2O6 at 7 GPa, have been investigated. Quantitative analysis leads to the following formulae: (Ca0.75K0.23Mg0.02)(Mg0.73Al0.27)(Si1.97Al0.03)O-6.00 and (Ca0.90K0.07 Mg-0.03)(Mg0.86Al0.14)(Si1.94Al0.06)O-6.00, for K1 and K2 respectively. Lattice parameters are: a = 9.803(2), b = 8.985(2), c = 5.263(1) Angstrom, beta = 105.69(1)degrees for K1 and a = 9.744(1), b = 8.904(2), c = 5.273(1) Angstrom, beta = 106.14(1)degrees for K2. The structures were refined to R-all = 1.16 and 2.02 %, respectively, using 982 independent reflections. Substitution of K for Ca causes strong modifications to the average structure, mainly a lengthening of the M2-O3C1 bond distance and a shortening of the T-O3A1 bond distance. The crystal K1 shows the largest volume for a M2 polyhedron ever reported for the clinopyroxene structure with divalent cations in this site. No evidence was found for a small cation such as Mg coexisting with Ca in the M2 site that might act as a structural stabilizer for the accommodation of K in the clinopyroxene structure.
引用
收藏
页码:929 / 934
页数:6
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