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Figure 3
Structure of γ-SiO2 stishovite. The shaded plane is the (110) plane, which is composed of equatorial oxygen atoms of O1 and O2 in the rutile structure.

Journal logoJOURNAL OF
SYNCHROTRON
RADIATION
ISSN: 1600-5775
Volume 12| Part 5| August 2005| Pages 566-576
doi:10.1107/S0909049505022016
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