Another possibility is that the sinking plate cools the neighboring mantle and produces convection currents that move the plates.
另一种可能是下沉的板块冷却了邻近的地幔,并产生对流,使板块移动。
It seems possible that a sinking current of cooled mantle material on the upper side of the plate might be the cause of such deep basins.
看来,板块上侧冷却的地幔物质的下沉流可能是造成这种深盆地的原因。
An alternative theory is that the sinking part of the plate, which is denser than the hotter surrounding mantle, pulls the rest of the plate after it.
另一种理论是,板块下沉部分的密度大于周围较热的地幔,将板块的其余部分拉在后面。
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