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。
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.
地幔的运动类似于一壶沸水的运动,它把热的物质带到表面,再把较冷的物质带到深处,从而使地幔冷却。
The mantle's motions, analogous to those in a pot of boiling water, cool the mantle by carrying hot material to the surface and returning cooler material to the depths.
当气体冷却,任何有毒的物质会被封在玻璃状的熔渣中,被安全的填埋。
When the gas is cooled, any hazardous elements in the waste end up sealed in a glassy slag that is safe to put into landfill.
We show particles interacting with the colon collisions.
我们想表现物质和冷却剂的,互动过程。
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