根据滑移线场运动学可容条件的要求，推论出在第一变形区与第二变形区之间及第一变形区与第三变形区之间存在着另外两个变形区。
It's deduced that besides the three deformation zones, other two deformation zones must exist according to the kinematical admissibilities of the constructed slip-line field.
正如同极相斥，而这两个场之间的排斥力强到足以使那块金属变形。
Like poles repel, and the repulsion between the two fields is strong enough to make the metal distort.
在这之后两个月间，北侧山体变形并出现一个巨大的隆起——这是底部岩浆上涌，岩石被推起来的标志。
Over the next two months, the northern flank of the mountain was deformed by a large bulge-a sign that upwelling magma was pushing up on the rock from below.
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