亚洲中部和东部强烈而广泛分布的地震活动被认为是印度板块和亚洲板块之间碰撞的直接结果。活动的亚洲大陆的重大变形是巨大的走向滑动断层引起的,这些断层导致“瞬时”构造运动。并且使发生碰撞的印度板块之前的亚洲地壳和岩石圈受挤压向一侧,主要向东运动。模型的基本作法用—“刚体”(印度)挤压—“塑性体”(亚洲)。平面塑性应变理论在某种程度上可成功地予测瞬时运动,几何形态与不同的挤压体引起的应力场以及大体上与印度一欧 Strong and widely distributed seismic activity in central and eastern Asia is considered as a direct result of the collision between the Indian and Asian plates. Major deformations of the active Asian continent are caused by the tremendous strides towards slip faults that lead to “momentary” tectonic movements. And to crush the Asian crust and lithosphere that preceded the impacted Indian plate to one side and move mainly eastward. The basic idea of ​​the model is to use - “rigid body” (India) extrusion - “plastic body ” (Asia). The plane plastic strain theory can, to some extent, predict the instantaneous motion, the stress field caused by geometries and different extrusions, and in general,