The collision between the two plates is mainly controlled by Tancheng-Lujiang Fault Zone.
郯庐断裂在两板块碰撞事件中起了主控作用。
The foreland sediments and structures also show the activity of the fault zone during the collision of the North and South China plates.
前陆沉积与变形构造也表明该断裂带在华北与华南板块碰撞中就发生了活动。
The stitching pluton, intruded into main fault plane of collision zone, could be formed in syntectonic period and also in the period of subsequent collision, i. e. post collision.
沿碰撞带主断层面贯入的“钉合岩体”可以是同构造期形成的，也可能是继续碰撞作用的产物。
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