1. Olivine-spinel transition in the system Mg2SiO4-Fe2SiO4, at 800°C;Akimoto;Earth Planet. Sci. Lett.,1966
2. The system MgO-FeO-SiO2 at high pressures and temperatures -phase equilibria and elastic properties;Akimoto,1972
3. High-pressure crystal chemistry of orthosilicates and the formation of the mantle transition zone;Akimoto,1976
4. High-pressure transformation in Co2SiO4 olivine and some geophysical implications;Akimoto;Phys. Earth Planet. Interiors,1968
5. Iron-magnetism distribution coefficients between spinel [(Mg,Fe)2SiO4], magnesiowüstite [(Mg,Fe)O], and perovskite [(Mg,Fe)SiO3];Bell;Carnegie Inst. Washington Yearb.,1979