岛弧形成于两个板块之间的活跃边界上，其中一块会被推挤到另一块的下方(称之为“消亡”)。
Island arcs form along an active boundary between two tectonic plates, with one being driven beneath the other (subduction).
在下方的这幅图像里，你可以看到在浮油的边界上有两条船他们大概是在做控制和清理的努力。
In the image below, ships, presumably involved in the containment and cleanup efforts, can be seen near the edge of the slick.
似乎有很多的小火山，以减轻下方，而不是仅仅在为地球上的板块边界地壳岩浆的压力。
It seems to have many small volcanoes to relieve the stress of the magma beneath the crust rather than just at the plate boundaries as on the Earth.
你会注意到最下方的椭圆伸出了大圆圈的边界。
You will notice that the shape on the bottom extends the border of the big circle.
给出了分子流扩散方程的边界条件，推导出入口压力在线性近似下方程的解。
The molecule flow diffusion equation and the boundary conditions are given. The solution with linear approximation of entrance pressure is presented.
给出了分子流扩散方程的边界条件，推导出入口压力在线性近似下方程的解。
The molecule flow diffusion equation and the boundary conditions are given. The solution with linear approximation of entrance pressure is presented.
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