一般认为，转换带地震不连续面主要与橄榄石的高压相变密切相关。
The seismic discontinuities in transition zone are generally interpreted in terms of phase transformations in olivine component at high pressures.
一般认为，转换带地震不连续面主要与橄榄石的高压相变密切相关。
The seismic discontinuities in transition zone are generally interpreted in terms of phase transformations in olivine component at high pressures.
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