1) Altyn collisional orogenic belt
阿尔金碰撞造山带
1.
The displacement of Altyn nappe-strike slip fault system since the Meozoic modifies the former Altyn collisional orogenic belt,which resulted in the formation of a series of Jurassic sedimentary basins within the Altyn Mountain and the southeastern part of the Tarim basin.
阿尔金构造带包括阿尔金碰撞造山带和阿尔金逆冲-走滑断裂系。
2) 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。
3) 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。
4) collisional orogenic belt
碰撞造山带
1.
On the basis of geological studies of some 28 localities of Ultrahigh-Pressure Metamorphic (UHPM) rocks all over the world it is not difficult to find that most UHPM belts are developed in close relationship with the island arc-continent and the continent-continent collisional orogenic belts.
对全球28个超高压变质岩产地的地质对比研究发现,超高压变质带的发育,与弧-陆和陆-陆碰撞造山带关系密切。
2.
In a collisional orogenic belt,the strength of crust-mantle interaction is also positively correlated with metallogeny;especially in a multi-stage collisional orogenic belt,crust-mantle interaction was stronger and the belt contains abundant mineral resources.
碰撞造山带的壳幔物质相互作用与成矿作用的强度也呈正相关关系,特别是多期次碰撞造山带,均发生过强烈的壳幔物质相互作用,孕育着丰富的矿产资源。
5) collisional orogen
碰撞造山带
1.
Tectonic evolution of the western segment of the Altyn Tagh collisional orogen, Northwest China.;
阿尔金碰撞造山带西段的构造特征
2.
A collisional orogen formed in the Early Paleozoic is well preserved on the northern margin of the Qaidam basin.
柴达木盆地北缘在早古生代形成了一条碰撞造山带,该造山带结构保存较完整,可分辨出深俯冲板片、火山岛弧带、蛇绿杂岩带、岛弧深成岩带等组成单元。
3.
The northwest-trending Early Paleozoic collisional orogenic belt located on northernmargin of the Qaidam basin is a part of the Central Orogenic belt and one of a few places inChina where HP-UHP metamorphic rocks exposed.
柴北缘早古生代碰撞造山带呈北西向展布于祁连山与柴达木盆地之间,是我国中央造山带的重要组成部分,也是我国仅有的几个存在高压-超高压变质岩的地点之一。
6) Altun orogenic belt
阿尔金造山带
1.
The inversion for the Q value of the upper crust along the profile from Baicheng to Da Qaidam has been carried out using seismic reflection/refraction data acquired on the profiles which cross the Tarim basin, the Altun orogenic belt and the Qaidam basin, respectively.
利用横跨塔里木盆地、阿尔金造山带和柴达木盆地的拜城—大柴旦综合地球物理剖面的人工地震宽角反射 折射资料 ,对拜城—大柴旦剖面研究区上地壳的Q值结构进行了反演 。
补充资料：山带
1.指环绕峰岩的带状白云。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条