燕山期，全面陆-陆碰撞期间其主要表现为脆性变形特征。
The brittle deformation mainly occurred in the nouthern part during continent-continent collision in the Yanshanian epoch.
摘要：亚特拉斯山和阿特拉斯山是与已存在和仍在发育的陆-陆碰撞相连的褶皱带。
The High Atlas and the Anti Atlas are fold-belts linked to former and still ongoing continent–continent collisions.
东准噶尔双泉一带的韧-脆性剪切带是在板块结合带基础上，形成于陆-陆碰撞体制。
Basing on the combination of plates, ductile-brittle shear zone in the ShuangQuan area, Eastern JungGar forms in the system of continental - continental collision.
早石炭世末，准噶尔-哈萨克斯坦与西伯利亚板块发生陆-陆碰撞，形成大型双重逆冲推覆构造。
The continental collision between Siberian and Kazakhstan-Junggar in Early Carboniferous shaped the large-scale dual thrust-nappe structures in the Altay orogen, NW China.
山脉是大陆板块之间的碰撞导致陆地上升而形成的。
Mountains are built by the collisions between continental plates that force land upwards.
大约5500万年前就开始的非洲大陆及欧洲大陆的相互碰撞形成了阿尔卑斯山。
The formation of the Alps through the collision of the two continents Africa and Europe began about approximately 55 million years ago.
斗罗大陆因为四千多年前被西方大海漂浮而来的日月大陆碰撞，面积大增的同时，也令大陆战事频繁。
Douro mainland because Western sea floating to the continental collision was four thousand years ago, increased area at the same time, also makes frequent wars.
尤其是四千多年前那次地壳变动引来的大陆碰撞，不但令斗罗大陆面积增大了超过一倍，同时也带去了许多变数。
Especially four thousand years ago that the crustal movements of continental collision event, not only make the Douro mainland area increased more than one times, but also brought many variables.
四千至五百万年前，印度大陆漂移与欧亚大陆发生碰撞，喜马拉雅山脉隆起。
Between 40 and 50 million years ago, India drifted right into Eurasia, raising the Himalayan Range.
印度—亚洲大陆的碰撞所形成的向东和东南的地幔流可能推动了东亚大陆东侧和南侧俯冲带的后退，并引发弧后扩张作用。
The eastward or southeastward mantle flow resulting from the collision of IndiaEurasia probably pushed rollback of slabs east and southeast to east Asian continent, further causing back arc spreading.
它的形成主要受地热条件的控制。麻粒岩的形成可以与大陆碰撞、大陆拉张以及大陆弧模式相联系。
Its formation was controlled mainly by the condition of terrestrial heat. Their main formation models are related to continental collision, continental extension and continental arc.
与弧背前陆盆地和周缘前陆盆地相并列，并对应于板块构造演化历程中的大洋消减、大陆碰撞和陆内缩短三个不同性质的聚敛阶段。
Therefore they are corresponding to the three different featured convergent stages of ocean subduction, continental collision and intra-continent contraction in the structural evolution of plates.
表明印度板块对中国大陆碰撞力最大，其次是菲律宾海板块对中国大陆的俯冲力。
According to the estimation, the impact force from India plate to China's continent is the maximum, and then is the underthrusting force from Philippine Sea plate to China's continent.
侏罗纪—新生代在三叠纪碰撞基础上，太平洋板块向欧亚大陆连续俯冲和加积，进而形成由三叠纪—新生代杂岩组成的欧亚大陆东部地区的巨大加积杂岩带。
Following the Triassic collision, with Pacific plate subduction and continuous accumulation towards Eurasian plate in the Jurassic-Cenozoic, the huge accretionary complex belt was eventually formed.
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.
大陆与大陆沿俯冲带的碰撞使大陆扩大，而沿扩张中心的断陷使它们再次分开。
Continent to continent collisions along subduction zones makes continents larger, while rifts along spreading centers break them apart again.
印度次大陆从南极洲脱离，漂过印度洋越过喜马拉雅山与亚洲陆块猛烈碰撞；
The Indian subcontinent detaching itself from Antarctica and sweeping across the Indian Ocean to its violent collision with Asia's landmass across the Himalayas;
沿江前陆盆地形成于扬子与华北板块碰撞活动中的前陆变形带上。
The around-Yangtze foreland basin occurred in a foreland deformation belt caused by the collision between the Yangtze and North China plates.
滇西北拖顶地区斜向走滑构造是金沙江再生小洋盆关闭、陆-陆斜向碰撞构造转化的结果。
The oblique strike slip structure is resulted from the closing of little Jingshajiang regeneration ocean basin and the oblique intercontinental collision in late Triassic.
滇西北拖顶地区斜向走滑构造是金沙江再生小洋盆关闭、陆-陆斜向碰撞构造转化的结果。
The oblique strike slip structure is resulted from the closing of little Jingshajiang regeneration ocean basin and the oblique intercontinental collision in late Triassic.
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