1.
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
2.
IDENTIFICATION OF SOUTHEASTERN FUJIAN MESOZOIC COLLISIONAL OROGENIC BELT
闽东南中生代碰撞造山带的确认证据
3.
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?
4.
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
5.
The frequency dispersions of Rayleigh waves and 3-D velocity structures in Himalayan collision orogenic zone and Qiangtang basin
喜马拉雅碰撞造山带和羌塘盆地的瑞雷波频散与三维速度结构
6.
The Metallogeny of the Miocene Gangdese Porphyry Copper Belt in Tibetan Collisional Orogen;
西藏碰撞造山带冈底斯中新世斑岩铜矿成矿作用研究
7.
The deformation characteristics of Longquanguan DSZ reflect the tectonic evolution of the late Archaean collision orogenic belt in Wutaishan area.
龙泉关韧性剪切带的变形特征反映了五台山晚太古代碰撞造山带的构造演化。
8.
THE CHARACTERISTICS OF THE METAVOLCANIC ROCK SERIES OF EARLY PALAEOZOIC ERA AND THE STRUCTURAL ENVIRONMENT OF THEIR GENESIS IN THE NORTHERN PART OF THE EAST QINLING-TONGBAI-DABIE COLLISION TYPE OROGENIC BELT
东秦岭-桐柏-大别山碰撞造山带北部早古生代变质火山岩系特征及其形成环境
9.
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
10.
Shrinking History of Archipelagic Island-arc-basin System in the Plate Junction in the West Songpan-Ganzi Orenic Zone during the Mesozoic
松潘-甘孜造山带西部碰撞结合带中生代多岛弧盆收缩史
11.
Preliminary Study of Breakup Process of the Plate Junction in the West Songpan-Ganzi Orogenic Zone during the Paleozoic
松潘-甘孜造山带西部碰撞结合带古生代裂解史初探
12.
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。
13.
Porphyry Cu deposits in collisional orogen setting:A preliminary genetic model
初论碰撞造山环境斑岩铜矿成矿模型
14.
VOLCANO-MOLASSE GEOLOGICAL STRUCTURE AND GEOCHEMICAL SIGNATRE IN DEVONIAN PERIOD COLLISION OROGENIC IN BEISHAN,GANSU-INMONGOLIA
北山泥盆纪碰撞造山火山－磨拉石地质构造及地球化学特征
15.
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。
16.
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。
17.
Early Paleozoic Collisional Orogeny and Magmatism on Northern Margin of the Qaidam Basin
柴达木盆地北缘早古生代碰撞造山及岩浆作用
18.
Present Hydrothermal Activities during Collisional Orogenics of the Tibetan Plateau;
青藏高原碰撞造山过程中的现代热水活动