A re-investigation on structural stability of CaGeO3 perovskite was conducted by synchrotron radiation X-ray diffraction with diamond anvil cell up to 48.8 GPa and first-principles calculations based on density functional theory. Both experimental and theoretical results reveal that CaGeO3 perovskite becomes more distorted deviated from the ideal perovskite with increasing pressure, in contradiction to previous experimental results. A phase transition from perovskite to post-perovskite of CaGeO3 is theoretically predicted to occur at 36-44 GPa, which is experimentally observed at 43 GPa quenched from high temperature. Elastic behavior of CaGeO3 at high pressures is similar to those of MgSiO3. A large positive jump (+4%) of shear velocity in CaGeO3 is predicted across the phase-transition pressure. Crown Copyright (C) 2011 Published by Elsevier B.V. All rights reserved.
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Japan Agcy Marine Earth Sci & Technol, Inst Res Earth Evolut, Yokosuka, Kanagawa 2370061, Japan
Univ Tokyo, Earthquake Res Inst, Bunkyo Ku, Tokyo 1130032, JapanJapan Agcy Marine Earth Sci & Technol, Inst Res Earth Evolut, Yokosuka, Kanagawa 2370061, Japan
Ono, Shigeaki
Kikegawa, Takumi
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High Energy Accelerat Res Org, Tsukuba, Ibaraki 3050801, JapanJapan Agcy Marine Earth Sci & Technol, Inst Res Earth Evolut, Yokosuka, Kanagawa 2370061, Japan
Kikegawa, Takumi
Higo, Yuji
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Japan Synchrotron Radiat Res Inst, Sayo, Hyogo 6795198, JapanJapan Agcy Marine Earth Sci & Technol, Inst Res Earth Evolut, Yokosuka, Kanagawa 2370061, Japan