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.
它们常常把小海象留在浮冰上，以避免陆地上拥挤海象群的碰撞。
They often keep their young on ice floes to avoid the crush of the jostling walrus crowds on land.
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.
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.
他最近的著作《回到泰坦尼克号》，谈及潜水器碰撞及登陆沉船而造成损害的证据：船头有道深深的裂口，桅杆和守望塔严重腐烂，桅杆钟已被移走。
His recent book, Return to Titanic, includes evidence of damage caused by submersibles hitting and landing on the ship. There is a gash to the bow.
大约在6550万年以前，也就是在白垩纪末期，地球与一颗小行星发生碰撞，此后这种史上陆地最大的动物便由此绝迹了。
Some 65.5m years ago, at the end of the Cretaceous period, the Earth collided with an asteroid and the biggest terrestrial beasts in history were no more.
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.
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.
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.
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.
之所以如此，显然与山东所处的大地构造位置，即太平洋板块与欧亚板块相互碰撞的陆缘地带密切相关。
This is apparently related to the tectonic setting of Shandong, namely, the continental margin where the Pacific Plate collided against the Eurasian Plate.
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.
从区域构造的观点看，同板块碰撞有关的前陆盆地是油气聚集的有利地区。
From a tectonic point of view, foreland basins related to plate collision are areas favorable for petroleum accumulation.
中部韧性层在南阿尔卑斯和欧洲前陆碰撞过程中，既有垂向挤出，也有侧向挤出。
In the process of south Alps Europe foreland collision, not only the vertical extrusion, but also the lateral extrusion develops.
前陆沉积与变形构造也表明该断裂带在华北与华南板块碰撞中就发生了活动。
The foreland sediments and structures also show the activity of the fault zone during the collision of the North and South 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.
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.
曾母盆地是南沙块体向南俯冲与婆罗洲块体发生软碰撞而形成的一个周缘前陆盆地，经历了四个不同的构造演化阶段。
Zengmu basin is a peripheral foreland basin, formed from southern subduction of Nansha Block and gentle collision with Borneo Block, and experienced four stages of tectonic evolution.
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.
目的是借鉴克拉通化概念和研究问题的思路对碰撞后和陆内阶段的构造岩浆作用的规律做一讨论。
The aim of this paper is to approach the rules of tectonomagmatic actions after the collision and in the intercontinental stage on the basis of the conception of the cratonization.
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.
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.
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.
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.
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