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Science (New York, N.Y.)
|June 24, 1994
PubMed
概括

地球地幔中的螺旋-矿相位过渡从负向正的Clapeyron斜率在2000°C以上转移. 这种变化阻碍了寒冷的下流,但允许热升起,从而产生部分层叠的地幔对流.

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