对流翻腾,湖水对流;
Because of its special physical and chemical properties, the continental lithosphere does not actively take part in the convective mantle overturn. However it influences the convective flow and vice versa.
由于其特殊的物理化学性质,大陆岩石圈通常不直接参与下方的地幔对流,但其与地幔对流格局有着重要的相互影响。
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