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碰撞构造     
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  collision tectonics
     STUDY ON COLLISION TECTONICS IN THE EAST ASIA:TANLU-SHANGTAER COLLISION ZONE
     亚洲东部碰撞构造:郯庐—尚塔尔碰撞带研究
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     This is a complex collision tectonics region of Precenoozic terranes, which can be divided into several elements from west to east, as follows: northwest Fujian terrane, Longquan collision zone, southeast Zheijiang、terrane, costal collision zone and Wen Don terrane.
     本区是一个前新生代地体碰撞构造区,由西往东有下列地体及地体碰撞带:闽西北地体,龙泉碰撞带,浙东南地体,东南沿海碰撞带,温东地体。
短句来源
     THE COLLISION TECTONICS OF THE KUNGGARTAG AREA IN THE EAST OF THE NORTHERN TIANSHAN
     北天山东段康古尔塔格碰撞构造
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     CRITICAL EXAMINATION ON CONTINENTAL COLLISION TECTONICS
     大陆碰撞构造剖析
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     Based on the theory of collision tectonics, orogenic blet and basin analysis, this paper studies the sedimentary response of collision process in the mid-Bangonghu-Nujiang Suture Zone.
     本文运用碰撞构造理论、造山带与盆地分析方法,研究了班公湖—怒江中段安多地区晚中生代碰撞作用过程的沉积响应。
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  collisional structure
     The Moho that underthrusts beneath the Dabie orogen and the south-dipping reflections of southern Dabie create a crossed reflection image, depicting the collisional structure beneath the collision of the Yangtze foreland and Dabie orogen.
     莫霍面向北插入大别山造山带下与南大别山地壳内南倾反射震相叠置,构成交叉反射图像,刻画出扬子前陆与大别山造山带的碰撞构造面貌。
短句来源
  collision orogeny
     By means of geochemical and geobarometric methods, it is estimated that the depth of emplacement for Jinjiling batholith was about 6.5km, and the rock forming pressure was about 180MPa. Jinjiling composite granitic batholith belongs to S type granitoids, forming in collision orogeny environment.
     采用地质地球化学方法估算出金鸡岭岩基的侵位深度约为 6.3km ,成岩压力为 180MPa ,具中深成相特征 ,属S型花岗岩并形成于华南板块内部的碰撞构造环境。
短句来源
  collisional structures
     COLLISIONAL STRUCTURES AND BASINAL DEFORMATION IN THE NORTH QAIDAM BASIN
     柴达木盆地北部碰撞构造与盆地改造变形
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  collision tectonics
Regional metamorphism related to collision tectonics in the Late Carboniferous (Hercynian) and later during the Alpine orogeny, caused intensive recrystallization and partial mobilization of the various carbonate phases.
      
The mineralising event is interpreted as relating to input of deep-sourced fluids during late-orogenic exhumation at the transitional stage between collision tectonics and the late-Variscan extensional regime.
      
The collision tectonics of the southern Greek Neotethys
      
Eastern European alpine system and the Carpathian Orocline as an example of collision tectonics.
      
They are useful information for understanding the collision tectonics of the Taiwan Island.
      
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  collisional structure
Vendian metamorphism in the accretionary-collisional structure of central Asia
      
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