印度洋板块

其应力分布主要受菲律宾海板块和印度洋板块的影响。

The distribution of stresses is chiefly effected by philippine Sea Plate and Indian Ocean Plate .

同时求得东构造结区由高密度的刚性物质构成，在印度洋板块的碰撞、挤压作用下呈向北运移，并插入青藏高原东缘。

The ' east structural knot ' is composed of high-density matter , moves northward after the collision and extrusion by the Indian Ocean plate , and then inserts into the eastern margin of the Qinghai-Xizang Plateau .

边界条件主要考虑了印度洋板块和太平洋板块对欧亚板块的挤压作用。

Some boundary loading is applied as convergence of Eurasia plate with Pacific plate and indian plate .

在非洲板块和欧亚板块的印度洋板块边界、地震也不断。

In the Eurasian plate , African plate and the Indian Ocean plate boundary , Earthquake never interrupt .

早白垩世晚期该区受太平洋板块和印度洋板块俯冲作用影响，华北板块再次转入挤压作用阶段，开始了滨太平洋域的演化。

In the late early Cretaceous , the NCC turned into contraction stage again by the influence of the subduction of Pacific plate and Indian plate .

南岭成矿带是太平洋及印度洋板块对中国大陆板块联合作用的结果。

The Nanling metallogenic belt is the result of the combination of the Pacific plate and the Indian oceanic plate with the continental plate of China .

这是印度洋板块向北推挤碰撞的作用力与反作用力，明显大于太平洋板块对欧亚板块的作用力与反作用力的结果。

The reason is that the action force and reaction force of India plate push toward north obviously is larger than the action force between the two plates .

研究的初步结果表明，印度洋板块与欧亚板块交接地带的北界为雅鲁藏布江，南界为恒河平原的北缘。

The preliminary results indicate that the northern boundary of the zone where Indian plate and Eurasian plate are in contact is Yarlung Zangbo River and the south-ern boundary is in the northern edge of Ganga plain .

羌塘地块、拉萨地块及喜马拉雅地体和印度洋板块向北漂移与欧亚大陆的拼合是柴北缘盆地形成演化的主要动力来源。

The Qiangtang block , the Lhasa block , the Himalayan block and the Indian plate drift northward and combine with the Eurasian continent , which are the main power sources of formation and evolution of the northern margin of Qaidam Basin .

考虑了五种应力和位移边界条件，这些边界条件分别反映了印度洋板块、太平洋板块及菲律宾海板块对我国及邻区施加应力的相对大小。

Five models of boundary conditions of stress and displace-ment have been considered , which represent relative values of the stress applied to the region inside China and its vicinity by the Indian ocean plate , the Pacific plate and the Philippine sea plate respectively .

总体结果表明，中国大陆及其周缘岩石圈应力场和构造运动可以归结为印度洋板块、太平洋板块、菲律宾海板块与欧亚板块之间相对运动，以及大陆板内区域块体之间的相互作用的结果。

The results suggest that the stress field of the lithosphere and tectonic movement in and around continental China are attributable to the motions of the Eurasian plate relative to the Indian , Pacific and Philippine Sea plates and interactions among blocks within the continental plate .

根据亚洲东南部地块的震源应力场资料，认为本区应力场及其特征可以从太平洋板块和印度洋板块相对于欧亚板块的运动得到合理的成因解释。

Based on the stress field data of Southeast Asia from earthquake focal mechanism analysis , it seems clear that the stress field , as well as its character , may reasonably be explained by the movement of the Pacific and the Indian Ocean plates relative to the Eurasian Plate .

中亚蒙古大洋、秦祁昆大洋、古特提斯洋、中特提斯洋、印度洋以及印度板块等在不同地质时期的板块活动是中国中西部地区盆地演化发展的动力学因素。

The plate movements in different geological history phrases are the dynamics of basin evolution and development in the middle and western parts of China .

从板块构造观点看来，南海及其周围整个东南亚大陆边缘恰好位于欧亚板块、太平洋板块和印度洋-澳大利亚板块交汇处，即处于一板块“三叉点”上。

According to the concept of plate tectonics , the South China Sea and its surroundings , the Southeast asiaregion , is the site of a major " triple junction " between three plates & eurasian , Pacific and Indo-Australian plates .