1.
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
2.
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。
3.
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。
4.
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。
5.
TECTONIC EVOLUTION OF THE LATE ARCHEAN WUTAISHAN COLLISION OROGEN
五台山晚太古代碰撞造山带构造演化
6.
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；
7.
IDENTIFICATION OF SOUTHEASTERN FUJIAN MESOZOIC COLLISIONAL OROGENIC BELT
闽东南中生代碰撞造山带的确认证据
8.
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。
9.
South Tianshan: a Late Paleozoic or a Triassic orogen?
南天山:晚古生代还是三叠纪碰撞造山带?
10.
METAMORPHISM EVOLUTION OF THE LATE ARCHEAN COLLISION OROGENIC BELT IN WUTAISHAN
五台山晚太古代碰撞造山带的变质作用演化
11.
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
12.
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；
13.
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。
14.
Yanshanian Superposed Structural Characteristics of West Margin of Foreland Fold Belt of South Dabashan
燕山期南大巴山前陆褶皱带西缘叠加构造特征
15.
There was an orogenic belt called the Cathaysian continental marginal orogenic belt in late Mesozoic along the present northern margin of the South China Sea.
南海北部陆缘在中生代晚期曾形成宏伟的华夏陆缘造山带。
16.
Research on the Tectogenetic Movement and the Fluid Migration in Dabashan Thrust and Fold Belt and Its Foreland;
大巴山冲褶带及前陆构造活动与流体运移研究
17.
Geodynamic Processes of the Central Asian Orogenic Belt and Its Metallogeny
中亚造山带大陆动力学过程与成矿作用
18.
TECTONIC DEFORMATION FEATURES OF SHENNONGJIA REGION IN EASTERN DABASHAN FORELAND STRUCTURAL BELT
大巴山前陆带东段神农架地区构造变形研究