后碰撞弧 postcollisional arCS
造山后碰撞作用 post-orogenic collision
后碰撞型SP花岗岩 post-collision type SP granite
碰撞后消亡 Die After Collision
弧-陆弧后碰撞 back arc continent-arc collision
前后碰撞缓冲区域 Deformation zones front and rear
碰撞后产卵 Spawn on Collision
碰撞后 Random ; post-collisional
车辆碰撞后飞起 Cars Fly Away When Hit
碰撞后的守候 standing by after collision
岩石学、岩石化学、地球化学特征反映该岩体属后碰撞强过铝花岗岩。
Its petrology, petrochemistry and geochemistry feature show the intrusive is post - collision and strongly - peraluminous granite.
这些碱长花岗岩在成因类型上属a2型,形成于后碰撞的张性环境中。
The alkali feldspar granites studied belong to A2 on petrogenetic type, and should be formed in a post-collisional tensional environment.
两类花岗岩的稀土元素地球化学特征明显不同,这与其所处的不同后碰撞构造演化阶段密切相关。
The characteristics of two types of granites are different, since A type and I type granites which formed at different stage of the post-collisional period.
So what happens almost instantaneously after the collision, the electron up here falls back down.
所以在碰撞后,几乎同时,在这儿的电子又回去了。
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