临津江带和沃川带都不具有碰撞造山带的变质特征。
The Imjingang and Ogcheon belts do not exhibit any metamorphic characteristics of collisional orogenic belts.
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。
Altyn structural belt consists of collisional orogenic belt and thrusting strike-slip fault systems.
该蛇绿混杂岩带是义敦碰撞造山带大地构造相中的弧前混杂带相。
The ophiolite melange zone represents forearc melange facies of the Yidun collision orogens.
义敦岛弧碰撞造山带是特提斯-喜马拉雅巨型造山带中的一个复合造山带。
The Yidun arc collision-orogenic belt is a composue orogenic belt of the giant Tethys-Himalaya orogenic zone.
龙泉关韧性剪切带的变形特征反映了五台山晚太古代碰撞造山带的构造演化。
The deformation characteristics of Longquanguan DSZ reflect the tectonic evolution of the late Archaean collision orogenic belt in Wutaishan area.
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。
Because a collision orogenic belt has a complicated crustal structure, new methods have to be adopted for thermal state analysis.
海拉尔盆地乌尔逊-贝尔凹陷是叠置于内蒙-大兴安岭古生代碰撞造山带的中新生代盆地。
Urxun-Beier depression in Hailaer Basin is the Mesozoic-Cenozoic basin located in the Paleozoic orogenic belt in Inner Mongolia-Daxing'anling area.
UHPM记录了显生宙俯冲-碰撞造山带早期碰撞过程中的低热流梯度及陆壳的深俯冲作用。
HPM-UHPM registers the low thermal gradients and deep subduction of continental crust during the early stage of the collision process in Phanerozoic subduction-to-collision orogens.
北祁连地区的红土沟-川刺沟金矿床产于早古生代碰撞造山带中，是该造山带形成和演化的阶段性产物。
The gold deposit at Hongtugou-Chuancigou in the northern Qilian area occurs in an Early Paleozoic collision orogenic belt, is a typical ductile shear zone gold deposit.
笔者提出，具有典型意义的瑞士阿尔卑斯碰撞造山带的研究成果对于深入研究我国西部造山带有着重要借鉴作用。
The present paper holds that the achievements in research on collision orogens in the Alps, Switzerland are of importance to the thorough research on the orogenic belts in west China.
推测形成这种运动方式的原因是造山带闭合时的斜向碰撞和造山带前缘准噶尔地块的透镜体边界效应。
This is attributed to the oblique collision during closing of the belt and the lens-effect of the Junggar massif in front of the belt.
东昆仑造山带具有软碰撞、多旋回的特点，造山带内的沉积盆地具有多物源和不同的大地构造背景。
The eastern Kunlun orogenic belt shows characteristics of soft-collision and multi-cycles. The sedimentary basins inside it have multi-sources and different tectonic backgrounds.
巴罗型中压变质带与巴肯型低压高温变质带的成因与大陆板块边缘的碰撞造山及陆内造山作用之间有着紧密的联系。
The origins of barrovian type and buchan type of metamorphism are commonly associated with orogenesis at continental collisional margins or within plates.
这些伸展构造很显然是扬子克拉通和华北克拉通在三叠纪碰撞时，大别山造山带前陆位置岩石圈弯曲导致地壳上部产生非弹性变形的结果。
Such structure in the collision foredeep of the Dabieshan Orogen was resulted in inelastic extensional deformation of the conver side of the flexed plate aroused by lithospheric flexure.
这些伸展构造很显然是扬子克拉通和华北克拉通在三叠纪碰撞时，大别山造山带前陆位置岩石圈弯曲导致地壳上部产生非弹性变形的结果。
Such structure in the collision foredeep of the Dabieshan Orogen was resulted in inelastic extensional deformation of the conver side of the flexed plate aroused by lithospheric flexure.
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