它是由印度板块在缅甸微板块下移动时发生的大型逆冲事件引起的。
It was caused by a megathrust event as the India plate moved beneath the Burma microplate.
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.
本文认为华北地震是印度板块碰撞和太平洋板块俯冲联合作用下形成的。
The author holds that the earthquakes occurred in North China are caused by the collision of India plate and the subduction of Pacific plate.
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.
特提斯洋关闭和印度板块持续推挤是中国西部前陆盆地形成的构造动力学背景。
Closing of Tethys and continuous compressing and squeezing of Indian plate were the tectonic dynamics background for the formation of foreland basins in western China.
古近纪末期逆冲构造形成机制与印度板块向欧亚板块之下俯冲的远程效应有关。
The overthrust tectonics at the end of Paleogene are related to the remote effect of subduction of Indian plate beneath Eurasian plate.
古近纪末期逆冲构造形成机制与印度板块向欧亚板块之下俯冲的远程效应有关。
The formation mechanism of thrust tectonics in the Paleogene was supposed to be related to a far field effect caused by collision between the Indian and the Eurasian 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.
他们认为由于板块运动，印度板块向中国和尼泊尔下发挤压，因此珠峰能够长高。
They say that the mountain is becoming higher as India is gradually pushed beneath China and Nepal because of shifting continental plates.
晚三迭世开始，印度板块在特提斯洋壳上向北仰冲，并导致特提斯在始新世的关闭。
Since the beginning of the upper Triassic epoch, the Indian plate upthrusted to the north over the Tethys oceanic crust and led to the closure of the Tethys in Eocene epoch.
四川省位于印度板块和欧亚板块这两个大陆板块的交界处附近，特别容易发生地震。
Sichuan lies near the boundary of two tectonic plates, the Indian and Eurasian landmasses, making it a particularly quake-prone area.
由于澳洲板块和印度板块相连了，太平洋的收缩迫使将近60%的澳洲大陆沈入海下。
Pacific Compression forced nearly 60% of the continent underwater due to the Australian Plate being connected to the Indian Plate.
云南省位于青藏高原东南隅，是亚欧板块和印度板块汇聚、消减、相互作用的边缘地带。
Yunnan Province is located in the southeast of Qingzang Plateau. And it is the convergence and interactional zone of Asia-Europe plate and Indian plate.
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.
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.
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.
科学界普遍认为，青藏高原和喜马拉雅山是6500万年前向北漂移的印度板块与欧亚板块相撞而形成的。
Scientists believe that 65 million years ago, the Indian Plate moving north collided with the Eurasian Plate, and the upheaval saw the emergence of the Qinghai-Tibet Plateau as well as the Himalayas.
然后显示了印度，它的西边明显下沉了，印度板块向侧面倾斜了一些，在此进程中东印度升起。
Then over to India where the western side of India sinks significantly, the plate tipping sideways a bit, raising eastern India during this process.
因为亚洲南部大陆地壳边缘起始于赤道以北1800英里处，这意味着它一定受到印度板块的挤压。
Because the edge of southern Asian continent is 1800 miles away from the north of the equator, it means there must be an extrusion from Indian Plate.
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.
帕米尔地区碰撞构造的岩石与同位素年龄，记录了印度板块对亚洲板块的运动，经历了俯冲、碰撞和榨挤3个阶段。
The rocks and isotopic age of collisional structures in Pamir Plateau recorded the movement of Indian plate towards Asian plate, which passed through 3 stages of subduction, collision and squeezing.
结果表明亚洲大陆板块具有明显的顺时针旋转运动特征；印度板块和澳大利亚板块从西南方向对亚洲大陆板块进行挤压；
The result shows that Asian mainland plate rotates clockwise, and been extruded by Indian plate and Australian plate from south-west, while the stations in western Pacific Ocean move toward northwest.
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.
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.
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