琥珀就像老照片一样显示了在印度与亚洲大陆碰撞之前印度的生物是什么样子的。
The amber shows, similar to an old photo, what life looked like in India just before the collision with the Asian continent.
用三维有限单元模型模拟了印度—亚洲大陆碰撞在板内的力学效应。
A three dimensional elastoplastic model was established to explore the mechanical aspects of the India-Asia continental collision by finite element modeling.
在印度与亚洲大陆碰撞后，它的动物群就从印度跳到亚洲一直延伸到欧洲。
After the collision between India and Asia, its fauna was able to jump from India to Asia where it spread all over Europe," Professor Rust said.
两大陆碰撞后，仰冲运动结束，代之以印度板块对欧亚板块南缘的推挤。
After the collision of the two plates, the obduction movement was replaced by the pushment of the Indian plate towards the southern edge of the Eurasian plate.
中国大陆碰撞带是以结构复杂、形成过程复杂和物质成分趋于混杂为主要特征的。
The collision zones in China Continent are mainly characterized by complex structures, complex forming processes and mixed materials.
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.
文中重点介绍了乌拉尔—阿曼巨型线性构造带和阿尔卑斯大陆碰撞带的影像特征和地质意义。
In this paper, we put emphasis on the introduction of the image characteristics and geological significance of Urals-Oman giant lineament and Alps continental collision.
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.
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.
在青藏高原采集的大地电磁资料描绘了地壳中的主要局部熔融区域，其结果和大陆碰撞地球动力学模型的结果相一致。
Magnetotelluric data collected on the Tibetan Plateau have imaged a major zone of partial melting in the crust, that agrees well with geodynamic models for this continent continent collision.
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.
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.
在崎岖多石的地形下面，埋藏着岩石和化石，这有趣地说明远古时代的大陆板块碰撞，形成了现在的地貌、气候和植被。
The rocks and fossils buried in this rugged landscape tell an intriguing story of an ancient collision that shaped the modern topography, climate, and plant life.
这些新的地质和地球物理信息加之以往的发现可进一步量化大陆俯冲和碰撞的过程。
These new geophysical and geological information together with previous findings are ready to quantify the processes of continental subduction and collision.
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.
然而，这并不是新大陆惟一存在的文化碰撞。
However, these were not the only cultures clashing on this continent.
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.
地震照地表科学家的理解，是由于大陆架板块彼此挤压碰撞而形成的。
The earthquake as scientists upon my surface understand is due to the movements of the plates of continental shelves over and under one another.
对应每一旋回，喀喇昆仑地层区和塔里木地层区发育有被动大陆边缘盆地和碰撞造山两种类型的岩石组合。
For Kala Kunlun and Tarim, two kinds of rock associations, passive continental marginal basin and collision orogenic belt, are developed corresponding to each cycle.
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.
在印度板块向欧亚大陆俯冲碰撞过程中，产生一系列深大断裂带，形成大量CO2释放脱气点。
There are come into being a series of deep seated fault zone and a great deal CO2 degasification point through the collision between Indian and Asian plates.
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.
在华南大陆形成过程中，主要构造事件为两次碰撞、三次裂解的主体构造格局。
During the formation of the South China continent, the main tectonic events had two collisions and three crackings which formed the main body of structural framework.
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.
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.
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.
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