印度板块
- 网络the Indian Plate;india plate
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水平形变还表明,印度板块以49.8mm/a向北推进。
The horizontal deformation also indicates that Indian plate has driven northwards by a value of 49.8mm/a .
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地震层析对印度板块向北俯冲的认识
Seismic Tomographic Constraint on the Northward Subduction of the Indian Plate
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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 .
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结果表明,本区既受到来自太平洋-菲律宾海板块向NW方向的挤压作用,又受到来自印度板块向N向E的挤压。
The result shows that the extruding has been subject to both the Pacific-Philippines Sea Plate in the NW direction and the Indo Plate in the N and E directions .
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在26.5°N,97°E附近,板块边界的走向发生突变,并形成东倾的缅甸山弧俯冲带,但印度板块挤压造成的主压应力方向为NNE向。
At about 26.5 ° N , 97 ° E , the boundary of the two plates turned to the south and formed a subduction zone which dips to the east under Burmese arc , but it causes compression in NNE direction .
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2印度板块的北推碰撞引起的青藏块体持续NE向挤压运动所产生的构造应力场,是本区构造形变与地震蕴育的主控应力。
The tectonic stress field generated by the NE-trending continuous compressive movement of Qinghai-Xizang block due to the northward press and collision of India plate is the principal stress for the tectonic deformation and earthquake development in this area .
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但当周期T≥30s时,盆地西部快波方向发生了明显变化,说明印度板块碰撞对塔里木盆地西部下地壳与上地幔的影响明显减弱。
Notable changes of fast propagation direction can be detected in western basin at periods above 30s ; therefore , it becomes an indicator that the Eurasia-India collision effect on lower crust and upper mantle beneath the western Tarim basin is weakened clearly .
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这三个大地基本单元在构造上的差异可以从地壳追寻到上地幔200km深处,反映出印度板块和太平洋板块的不同运动。
The differences in the stuctures among the above three tectonic units are likely to extend from the crust down to 200 km deep in the upper mantle , this indicates the different movements of the Indian and Pacific ocean plates .
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在综合分析基础上,笔者认为印度板块与欧亚板块的碰撞启动时间在45Ma以后。
On the basis of an integrated analysis , the authors suggest that the collision between the India plate and Eurasian plate was initiated after 45 Ma .
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其演化和印度板块与欧亚板块的碰撞有关,具独特的发育特征和油气分布规律。
So it has unique development features and hydrocarbon distribution rules .
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印度板块的北缘在哪里?
Where is the northern margin of the Indian plate ?
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这两种裂谷机制都可归因于印度板块岩石圈的斜向俯冲作用。
This two mechanism all contribute to oblique subduction of India plate .
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从印度板块的漂移论喜马拉雅植物区系的特点
The Charateristics of Himalayan Flora in the Light of the Drifting of Indian Plate
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雅鲁藏布江断裂是印度板块与欧亚板块缝合线的置疑
Is the Yarlung Zangbo fault zone the suture between the Indian and Eurasian plates
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印度板块互相冲击
of Asia and India arecrashing intoeach other .
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印度板块北边界地震活动和中国大陆地震
Seismic activity along the northern boundary of Indian plate and earthquakes in china 's continent
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亚洲和印度板块之间的缓慢运动
The slow-motion crash between Asia and India
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该侧向排挤作用是由印度板块碰撞引起的。
Lateral expulsion resulted from the collision between the India plate and the Asian continent .
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印度板块-古亚洲板块碰撞及亚洲恐龙的出现
Collision between the Indian plate and the paleo-Asian plate and the appearance of Asian dinosaurs
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以上电性特征为研究印度板块和欧亚大陆碰撞机制提供了地球物理依据。
These important electrical characters provide important geophysical evidence for studying the mechanism of India-Eurasia collision .
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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 .
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且明显地受印度板块和太平洋板块所控制,以印度板块的作用为最强烈。
These movements are apparently constrained by Indian and Pacific plates , the former plays a dominant role .
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雅鲁藏布缝合带代表曾经存在于印度板块与亚欧板块之间的新特提斯古大洋残余。
The Yarlung-Zangbo surture zone marks the Neo-Tethyan remnants existed between the Indian plate and the Eurasian plate .
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而34篇中有20篇论文的注意力更集中于印度板块与欧亚板块相碰撞的深部过程。
Twenty of the 34 papers specialized in deep-seated processes of the collision of the Indian plate with the Eurasian plate .
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反映了该区的力源主要来自于印度板块与欧亚板块的碰撞。
It will be shown that the power source of this region is caused by the collision between India and Eurasia plate .
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印度板块和亚洲板块相撞是导致这些小岛从今天的巴基斯坦北部的海床上升起的原因。
Indian plate and Asia plate collision led to these islands from the northern part of Pakistan to rise on the seabed .
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星期一发生在中国四川的地震是印度板块和亚洲板块不断碰撞的结果。
The earthquake in the Sichuan Province of China on Monday was a result of a continuing collision between India and Asia .
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平均来看,75%以上的印度板块相对于欧亚板块间的南北向缩短是通过地壳增厚变形来吸收的,这意味着在调节整个青藏高原构造变形的过程中,逆断和地壳增厚起了主要的作用。
On the average , more than 75 % of the north-south shortening between India and Eurasia is absorbed by crustal thickening strains .
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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 .
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地震活动相关性定量方法及其在印度板块动力触角对中国西部地区地震影响中的应用
Quantitative Method of Relativity in Seismicity and Its Application to the Seismicity Influence of Dynamic Antennas of India Plate to West Part of China