作者: T. Yagi , H. K. Mao , P. M. Bell
DOI: 10.1007/978-1-4612-5683-0_10
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摘要: Recent laboratory data on high-pressure and high-temperature experiments of various silicates strongly suggest that silicate minerals having the perovskite-type structure are dominant phases in earth’s lower mantle (e.g., Liu, 1976; Mao et al, 1977). Discovery existence perovskites has naturally preceded knowledge their physical properties, thus no experimental have been reported so far elastic properties.