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1)  collisional and activated orogeny
碰撞活化造山
2)  collisional orogeny
碰撞造山
1.
In the tectonic evolution, large_scale migration and convergence of fluids towards foreland basins during collisional orogeny of the Yangtze and North China continental blocks were of vital importance in the formation of the metallogenic belt.
根据调查结果 ,结合前人资料 ,提出了大别碰撞造山过程中流体迁移汇聚与成矿的概念性模式。
3)  colliding activation
碰撞活化
1.
The FGD test rig is built up to investigate the colliding activation efficiency between the sorbent particles and spraying droplets in the prefixed alkaline spray generator and the effect of various factors on SO_2 removal efficiency.
提出了一种新的半干法烟气脱硫方法——多流体碱雾发生器烟气脱硫,运用两相流相似模化方法建立了烟气脱硫试验台,研究了该脱硫方法中CaO脱硫剂颗粒与雾化水滴的碰撞活化效率、脱硫效率以及各种因素对脱硫效率的影响。
4)  collision orogenic belt
碰撞造山带
1.
The late Archean collision orogenic belt in Wutaishan is situated in the central part of the North China Plate.
五台山晚太古代碰撞造山带由三个构造岩片组成,即南部构造岩片——弧前混杂岩带、中部构造岩片——岛弧系和北部构造岩片——弧后混杂岩带,其间以大型逆冲型韧性剪切带相拼合。
2.
Because a collision orogenic belt has a complicated crustal structure, new methods have to be adopted for thermal state analysis.
由于碰撞造山带具有的地壳结构的复杂性,必须采用新的研究方法来分析其热结构。
5)  collision orogen
碰撞造山带
1.
It is suggested in the paper that the Neoarchean collision orogeny in Wutai Mountain is with the character of oceanic crust subduction and continental-continental collision based on synthetic study of the slices, such as tectonic lithological combin.
通过对各岩片的构造岩石组合、岩石地球化学、变形变质作用和同位素年龄的综合研究,认为五台山地区新太古代碰撞造山带具有洋壳俯冲、陆—陆碰撞造山的特点。
2.
The Wutaishan collision orogen may be divided into three tectonic slices by applying the tectonic lithologic event method;from south to north they are the forearc mélange zone,paleoisland arc system and backarc mélange zone.
应用构造—岩性—事件法将五台山碰撞造山带划分为3个构造片体:弧前混杂岩带、古岛弧系和弧后混杂岩带。
6)  non-collisional orogeny
非碰撞造山
补充资料:碰撞活化
分子式:
CAS号:

性质:是质谱分析中用来研究离子组成的一种技术。用中性分子在质谱仪的无场区与离子碰撞,发生分子-离子反应,当碰撞气体的压力合适时,碰撞基本上不涉及动量转移,而是使反应离子的部分动能转变成内能。由于离子内能增加,可能发生高活化能的分解反应,导致原来的稳定的离子在无场区发生诱导分解。

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