大别山在中生代时期的造山运动是由于华北地块和扬子地块继晚元古代之后再次发生碰撞活动而发生的。
The orogeny of Dabie mountain was resulted from collision between the North China and Yangzi massifs in early Mesozoic. The tectonic evolution of Dabic orogenic bolt underwent two stages.
这就是那些发生造山运动和大地震的地区的情况，有点象撞车时碰撞点被破坏，而运动一定会停止。
This is in fact where mountain building and massive earthquakes occur, just as car crashes do their damage on the point of impact, when motion must stop.
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