Crystal structure of the high-pressure monoclinic phase-II of cristobalite, SiO2

被引:42
作者
Dove, MT
Craig, MS
Keen, DA
Marshall, WG
Redfern, SAT
Trachenko, KO
Tucker, MG
机构
[1] Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England
[2] Rutherford Appleton Lab, ISIS Facil, CLRC, Didcot OX11 0QX, Oxon, England
关键词
cristobalite; high-pressure; neutron diffraction; phase transitions;
D O I
10.1180/002646100549436
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
The crystal structure of the high-pressure phase-II of cristobalite has been solved by neutron diffraction (space group P2(1)/c, a = 8.3780(11) Angstrom, b = 4.6018(6) Angstrom, c = 9.0568(13) Angstrom, beta = 124.949(7)degrees, at P = 3.5 GPa). This phase corresponds to a distortion of the high-temperature cubic beta-phase, rather than of the ambient temperature and pressure tetragonal alpha-phase.
引用
收藏
页码:569 / 576
页数:8
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