仰冲板块（obducting plate，ascending plate）又称上冲板块（overriding plate）。洋壳板块上冲于大陆壳或过渡型地壳之上的过程称为仰冲作用，其中仰冲的洋壳板块为仰冲板块。
随着这些火山的生长，它们上升到海面以上会沿着仰冲板块的前缘形成岛链。
As these volcanoes grow, they rise above the ocean surface to form lines of islands along the leading edge of the overriding plate.
随着火山的成长变化，它们伸出海洋面，逐渐在仰冲板块的前沿形成一系列岛屿。
As these volcanoes grow, they rise above the ocean surface to form lines of islands along the leading edge of the overriding plate.
两大陆碰撞后，仰冲运动结束，代之以印度板块对欧亚板块南缘的推挤。
After the collision of the two plates, the obduction movement was replaced by the pushment of the Indian plate towards the southern edge of the Eurasian plate.
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