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该区域的垂直形变特征主要表现为山区上升、盆地下沉的继承性运动和山区下沉、盆地上升的逆继承性运动的相互交替的循环过程;
The vertical deformation feature of northeastern margin of Qinghai-Tibet block is a returns of the mountain go up, the basin go down and the mountain go down, the basin go up;
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