1.
The model for the subduction and collision of the Indian plate with the Eurasian plate and its implications for the tectonic evolution of the Qinghai-Xizang Plateau
印度板块向欧亚板块俯冲碰撞的新模式及其对青藏高原构造演化的影响
2.
Lithospheric Thermotectonic Simulation on the Indian-Eurasian Subduction and Collision
印度与欧亚板块俯冲-碰撞过程岩石圈热结构模拟
3.
Taiwan located in the southeastern brim of china mainland and it is a dive-collision singular island-arc zong from Filipine plate to Eurasia plate.
台湾地处中国大陆东南边缘是菲律宾海板块凸向亚欧大陆俯冲-碰撞异常岛弧带。
4.
The major dynamic mechanism of collision is the openning of Japanese Sea and Okhotsk sea and subduction of Philippine Plate.
碰撞的主要动力机制为日本海和鄂霍次克海的张开及菲律宾板块的俯冲。
5.
The deformational dynamics is controlled by the compressional settings which are caused by the minor-angle oblique subduction of the Izanagi Plate and the continent-to-continent collision betneen the Yangtze Plate and the North China Plate.
变形动力学受控于伊泽奈崎板块的小角度斜向俯冲和扬子板块与华北板块陆陆碰撞造成的挤压背景。
6.
Triassic magmatism in the southern Lancangjiang zone,southwestern China and its constraints on the tectonic evolution of Paleo-Tethys
滇西古特提斯俯冲-碰撞过程的岩浆作用记录
7.
The subduction system of the plate can be regarded as a factory.
板块的俯冲系统可以比拟为一个工厂。
8.
Study on Contact-impact Dynamic Response of the Die in Sheet Metal Stamping;
板料冲裁过程中模具的碰撞响应研究
9.
The temporal and spatial evolution of orogenic granitic belt shows certain kind of regularities: subduction type granites→collision type granites→extensional type granites.
造山带花岗岩的时空演变规律是：俯冲型→碰撞型→伸展型。
10.
Deep Subduction Erosion Model for Continent-Continent Collision of the Sulu HP-UHP Metamorphic Terrain
苏鲁高压—超高压变质地体的陆—陆碰撞深俯冲剥蚀模式
11.
As the plates move apart, they encounter other plates at their opposite sides.
当各块板块彼此分离时，他们又在对边与其它板块发生碰撞。
12.
Detailed Structure of the Subducting Slab under the Western Pacific Region;
西太平洋地区俯冲板块的精细结构研究
13.
THE PLATE SUBDUCTION AND STRESS STATE IN THE PAMIR-HINDU KUSH REGION
帕米尔—兴都库什地区板块俯冲及其应力状态
14.
As the plates move, they collide, move apart, or slide past one another.
当板块移动时，它们会发生碰撞、分离或滑动越过另一板块。
15.
Timing of the Transformation from Seafloor Spreading on the South Margin of the North China Block to Subduction within the North Qinling Orogenic Belt
从华北陆块南缘大洋扩张到北秦岭造山带板块俯冲的转换时限
16.
These new geophysical and geological information together with previous findings are ready to quantify the processes of continental subduction and collision.
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。
17.
Continent to continent collisions along subduction zones makes continents larger, while rifts along spreading centers break them apart again.
大陆与大陆沿俯冲带的碰撞使大陆扩大，而沿扩张中心的断陷使它们再次分开。
18.
Volcanoes and compressive deformation during collisions along subduction zones makes continents thicker, while erosion wears them down, making them broader and flatter;
沿俯冲带碰撞过程中的火山和压缩变形使大陆加厚，而侵蚀使它们消减，使之变平，变宽；