更新世，吕宋弧逆时针转动和弧陆碰撞阶段。
Stage 3, early Pleistocene, anticlockwise rotation of Luzon arc and continent-arc collision.
稀土元素地球化学研究为新疆准噶尔地区二叠纪后碰撞阶段的岩浆作用机理及地球动力学演化过程提供了重要证据。
The REE geochemical research has provided the important evidence for the mechanism of the Premian post-collision stage and the geodynamical evolution process.
碰撞有可能发生在理论上存在的两个“原月亮”冷却的最后阶段。
The collision would have taken place during the late stages of the theoretical proto-moons' cooling process.
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