Olivine-spinel transition in the system Mg2SiO4-Fe2SiO4 at 800°C
作者： Syun-iti Akimoto , Hideyuki Fujisawa
DOI: 10.1016/0012-821X(66)90076-8
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摘要: Abstract Olivine-spinel solid solution equilibria in the system Mg2SiO4-Fe2SiO4 have been studied over pressure range 45 to 92 kb at 800°C. The solubility of Mg2SiO4 spinel increases 27 mole % this range. corresponding olivine solvus was determined up 63 same interval.
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A. E. Ringwood, Merren Seabrook, Olivine-spinel equilibria at high pressure in the system Ni2GeO4-Mg2SiO4 Journal of Geophysical Research. ,vol. 67, pp. 1975- 1985 ,(1962) , 10.1029/JZ067I005P01975
A.E. Ringwood, The constitution of the mantle—II Geochimica et Cosmochimica Acta. ,vol. 15, pp. 18- 29 ,(1958) , 10.1016/0016-7037(58)90005-X
A.E Ringwood, The constitution of the mantle—I: Thermodynamics of the olivine-spinel transition Geochimica et Cosmochimica Acta. ,vol. 13, pp. 303- 321 ,(1958) , 10.1016/0016-7037(58)90032-2
Syun-iti Akimoto, Hideyuki Fujisawa, Takashi Katsura, The olivine-spinel transition in Fe2SiO4and Ni2SiO4 Journal of Geophysical Research. ,vol. 70, pp. 1969- 1977 ,(1965) , 10.1029/JZ070I008P01969