Chudinovskikh L, Boehler R. High-Pressure Polymorphs of Olivine and the 660 km Seismic Discontinuity [J]. Nature, 2001, 411: 574-577.
[6]
Shim S H, Duffy T S, Shen G. The Post-Spinel Transformation in Mg2SiO4 and Its Relation to the 660 km Seismic Discontinuity [J]. Nature, 2001, 411: 571-573.
[7]
Liudmila Chudinovskikh, Reinhard Boehler. MgSiO3 Phase Boundaries Measured in the Laser-Heated Diamond Cell [J]. Earth and Planet Sci Lett, 2004, 219: 285-296.
[8]
Kuroda K, Irifune T, Inoue T, et al. Determination of the Phase Boundary between Ilmenite and Perovskite in MgSiO3 by in Situ X-Ray Diffraction and Quench Experiments [J]. Phys Chem Miner, 2000, 27: 523-532.
[9]
Gasparik T. Phase Relations in the Transition Zone [J]. J Geophys Res, 1990, 95: 15751-15769.
[10]
Hirose K, Komabayashi T, Murakami M, et al. In Situ Measurements of the Majorite-Akimotoite-Perovskite Phase Transition Boundaries in MgSiO3 [J]. Geophys Res Lett, 2001, 22: 4351-4354.
[11]
Liu J, Zhao J, Che R Zh, et al. In Situ Energy Dispersive Diffraction under High Pressure Using Synchrotron Radiation [J]. Chinese Journal of High Pressure Physics, 2000, 14(4): 247-252. (in Chinese)