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1)  post-collisional period
后碰撞期
1.
The characteristics of these volcanic rocks suggest that they were produced in post-collisional period.
综合分析表明,这些火山岩形成于后碰撞期
2)  late conllisional period
碰撞后期
3)  volcanic rock of the post-collision
碰撞期后火山岩
4)  post-collision
后碰撞
1.
Metallogenesis in Tibetan collisional orogenic belt:Ⅲ. Mineralization in post-collisional extension setting;
青藏高原碰撞造山带:Ⅲ.后碰撞伸展成矿作用
2.
Based on tectonic and geochronologic analyses, the authors hold that large-superlarge gold deposits and Mesozoic granites in Jiaodong area are generated in both the compressional setting of post-collision between South China craton and North China craton and the shear setting of Izanaqi plate high-speed and oblique subduction as well as in late extension setting.
文章通过对大量前人构造地质学、同位素年代学等多元信息资料的分析,认为胶东中生代花岗岩和大型_超大型金矿床形成于华南_华北克拉通后碰撞挤压和伊泽奈崎板块快速斜冲剪切的双重构造环境及其后的拉张构造环境。
3.
They all belong to high-K, calk-alkaline, SP granites and are post-collisional SP granites of Mid-Late Jurassic age.
岩体侵位于昂孜错-色热巴断裂南北两侧,包含5次侵入事件,均属高钾钙碱性强过铝花岗岩类,是后碰撞型SP花岗岩,时代为中-晚侏罗世。
5)  Post-collisional
后碰撞
1.
Diverse post-collisional granitoids and their tectonic setting discrimination;
后碰撞花岗岩类的多样性及其构造环境判别的复杂性
2.
Geochemistry of the Carboniferous-Permian post-collisional granitic rocks from Tianshan;
天山石炭-二叠纪后碰撞花岗质岩石地球化学研究
3.
The post-collisional magma of late Paleozoic are widespread.
区内广泛发育晚古生代后碰撞岩浆岩,其中侵入岩年龄在328。
6)  Post-collision
碰撞后
1.
The post-collisional magmatism can provide a great deal of important information on the interaction of crust and mantle during subduction and collision.
碰撞后岩浆作用记录了俯冲/碰撞过程壳幔物质循环的诸多信息,其源区属性及所揭示的深部动力学背景对理解造山带构造演化和壳幔相互作用尤为重要。
补充资料:冰后期

晚更新世冰期结束之后的温暖时期,一般指全新世。1864年由福布斯(e.forbes)提出,认为莱伊尔(c.lyell)所称的更新世和现代,应分别称为冰期时代和冰后期。1885年国际地质会议通过更新世和全新世的名称。但有人认为,冰后期一词虽适用于晚更新世冰川发育区,但用于非冰川作用区未必合适;即使在欧亚、北美大陆冰川发育区,随着大冰盖的逐步消退,各地冰后期来临的时间也不相同。冰后期的气候、植被分期以北欧地区最有代表性,其分期方案从20世纪初期以来一直广为引用。

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