阿尔泰山东缘的新构造运动与强地震活动，除了与印度-欧亚板块碰撞作用有关外，可能还与局部地区的动力学过程有关。
So, the intense neotectonic movement and seismic activity on the eastern margin of Altai Mountains are related to the collision of India-Eurasia plate and maybe to the regional kinematic process.
中国西南地区的地震活动反映了由印度—欧亚板块碰撞引起的动力作用由西向东、由南向北的推进过程。
The earthquake activities in Southwest China reflect the eastward and northward progression of tectonic movements caused by the collision between the Indian and Eurasian plates.
这种差异性的隆升可能一方面与印度板块和欧亚板块碰撞的远程效应有关，另一方面也是更主要的原因可能受博格达山不同段深部差异性动力学过程所控制。
The difference in the uplifting may be because of collision between the Indian and Eurasian plates and also of being controlled by the processes of dynamics at different depths of Bogeda Mountain.
长期以来，甭哥正长岩体被认为是印度—欧亚板块碰撞引起的走滑剪切构造所控制的碱性岩浆活动的产物。
Bengge syenites has been always regarded as the product of alkaline magma activity controlled by the strike-slip structures caused by collision between Yindia and Euroasia.
印度板块往北，菲律宾板块往北西，太平洋板块往南西与欧亚板块碰撞的格局是中国地震构造的决定性因素。
The seismotectonic conditions in china are determined by the fact that the eurasian the indian the philippine and the pacific tectonic plates extend into its vicinity.
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.
青藏高原不是印度板块与欧亚板块碰撞的结果，而是形成于下地壳流动驱动的板内盆山作用。
The formation of the Qinghai-Tibet Plateau was not caused by the collision between India plate and Eurasia plate, but by intraplate basin-mountain coupling driven by lower crustal flow.
喜山早期，受印度板块与欧亚板块碰撞作用的影响，形成了北东—南西方向的水平挤压应力场。
During the Early Himalayan stage, the NE SW trending horizontal compressive TSF was formed by the effect of the collision of India plate and Eurasian plate.
这与印度板块和欧亚板块之间碰撞时代一致。
This is in accordance with the age of the collision between the Indian and Eurasian plates.
东构造结是印度板块和欧亚板块碰撞的奇点，历来是地学研究的热点。
The Eastern Himalayan Syntaxis is a singular point of continental collision between the Indian and Eurasian plates, and has been focused by many geoscientists.
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.
这一碰撞开始于5亿多年之前，当时印度之下的构造板块冲撞入欧亚板块。(略)。
This collision started more than 50 million years ago, when the tectonic plate beneath India crashed into the Eurasian plate. (Watch how the plates slammed into each other.)
准噶尔盆地南缘的晚新生代构造变形被认为是天山地区对印度和欧亚板块的碰撞与会聚作用过程的构造响应。
The late Cenozoic deformation is considered as a response to the India and Eurasia plate collision and continuous compression.
准噶尔盆地南缘的晚新生代构造变形被认为是天山地区对印度和欧亚板块的碰撞与会聚作用过程的构造响应。
The late Cenozoic deformation is considered as a response to the India and Eurasia plate collision and continuous compression.
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