Structure of Cu-bearing orthopyroxene, Mg(Cu.56,Mg.44)Si2O6, and behavior of Cu2+ in the orthopyroxene structure

被引:0
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作者
T. Tachi
H. Horiuchi
H. Nagasawa
机构
[1] Department of Chemistry,
[2] Gakushuin University,undefined
[3] Mejiro 1-5–1,undefined
[4] Toshima-ku,undefined
[5] Tokyo l7l,undefined
[6] Mineralogical Institute,undefined
[7] Faculty of Science,undefined
[8] University of Tokyo,undefined
[9] Hongo 7-3–1,undefined
[10] Bunkyo-ku,undefined
[11] Tokyo 113,undefined
[12] Japan,undefined
来源
Physics and Chemistry of Minerals | 1997年 / 24卷
关键词
Key words Cu2+-beearing orthopyroxene; Orthopyroxene; Crystal structure; Jahn-Teller effect;
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学科分类号
摘要
 Cu-bearing pyroxene, Mg(Cu.56,Mg.44)Si2O6, has been synthesized by a flux method and crystal structure refinement has been performed by single crystal X-ray diffraction. It is found that the crystal structure is orthorhombic (space group Pbca) with unit cell dimensions of a=18.221(4), b=8.890(1), c=5.2260(7)Å and the cell volume of 846.5( )3Å3. In the M2-site one of the M-O bonds(M-O3B) is extremely expanded from 2.444(2) in enstatite to 2.732(2), thus the coordination polyhedron around M2-site is regarded as square pyramidal rather than square planar or octahedral. It is also found that the M1-site in the pyroxene structure is occupied almost exclusively by Mg, while the M2-site is almost evenly occupied by Mg and Cu. The observed extreme site preference shown by Cu2+ is unusual among the divalent cations with similar ionic sizes.
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页码:463 / 476
页数:13
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