1.
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。
2.
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
3.
Stage3, early Pleistocene, anticlockwise rotation of Luzon arc and continent-arc collision.
更新世,吕宋弧逆时针转动和弧陆碰撞阶段.
4.
The end of the sedimentation of the foreland basin indicates completion of the collisional orogeny.
前陆盆地的终结标志着碰撞造山作用的结束。
5.
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。
6.
The deposition of the foreland basin and the intracontinental shortening are the response to the Indosinian collision and convergence between the Yangtze and Cathaysian blocks.
这些指示扬子和华夏陆块在印支期发生了强烈陆内碰撞与会聚及前陆盆地的沉积作用。
7.
The shear zone is a secondary structure zone of the syn-collision stage of Southern Tarim block with Ili-Isaik block.
该剪切带属南侧塔里木与伊犁－伊塞克两陆块碰撞缝合构造同碰撞期的次级构造带。
8.
Taiwan-Luzon arc, which is an arc-continental collision zone, is the south extremity.
冲绳海槽的南端为台湾-吕宋岛弧，为一比较典型的弧-陆碰撞构造带。
9.
LATE CENOZOIC NEOTECTONICS IN THE DONGSHA ISLANDS REGION AND ITS RESPONDS TO COLLISION BETWEEN CHINESE CONTINENTAL MARGIN AND LUZON
东沙群岛海区晚新生代构造特征及其对弧-陆碰撞的响应
10.
SHRIMP U-Pb Dating of Zircon from Gneiss in the Tongmai Region:Evidence for the India-Eurasia Collision Time
印度与欧亚两大陆块碰撞时间的厘定:来自锆石SHRIMP U-Pb年龄的证据
11.
The Indian subcontinent detaching itself from Antarctica and sweeping across the Indian Ocean to its violent collision with Asia's landmass across the Himalayas;
印度次大陆从南极洲脱离，漂过印度洋越过喜马拉雅山与亚洲陆块猛烈碰撞；
12.
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。
13.
A GRANULITE FACIES BELT OF THE MIDDLE-WEST PART EN NORTH MARGIN OF NORTH CHINA CRATON: AN EARLY PRECAMBRIAN CONTINENT- CONTINENT COLLISION OROGENIC BELT
一条早前寒武纪的陆-陆碰撞造山带——华北克拉通北缘中西部麻粒岩相带
14.
Late Archean Continent-Continent Collision Event of Middle Segment of North Margin of North China Plate:The Evidence from S-type Granite of Hejiao Area
华北板块北缘中段新太古代的陆-陆碰撞事件:来自合教S型花岗岩的证据
15.
The plane cracked up through a bad landing.
飞机因着陆不慎而撞毁。
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.
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；
18.
In the process of south Alps Europe foreland collision,not only the vertical extrusion,but also the lateral extrusion develops.
中部韧性层在南阿尔卑斯和欧洲前陆碰撞过程中 ,既有垂向挤出 ,也有侧向挤出。