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1)  Qilianshan Structure Belt
祁连山构造带
1.
The neotectonic deformation mechanism of Qilianshan Structure Belt;
祁连山构造带的新构造变形机制
2)  Qilian orogenic belt
祁连造山带
1.
The chemical compositions of the volatiles in mineral separates in harzburgite and dunite from the Yushigou ophiolite of Qilian orogenic belt,western China,were determined by stepwise heating mass spectrometer to reveal mantle fluids in ancient Qilian ocean.
为确定祁连古大洋地幔流体组成,采用分步加热质谱法测定了祁连造山带玉石沟蛇绿岩底部方辉橄榄岩和纯橄榄岩中的流体化学组成。
2.
The granitoids can be devided into three tectonics magma belts according to the petrochemistry and geochemistry study of Tianshui area located in the junction region between the Qinling orogenic belt and Qilian orogenic belt.
通过对地处祁连造山带与秦岭造山带结合部位的天水地区花岗岩类的岩石学、岩石化学、地球化学等资料的分析研究,区内花岗岩类可划分为3个构造岩浆带。
3.
Early Paleozoic ophiolitic suites preserved in Qilian orogenic belt give very great opportunities to emphasize insights into this scientific problem.
祁连造山带早古生代蛇绿岩单元内枕状玄武岩的元素、Sr-Nd-Pb同位素组成系统研究表明:其地幔源区的Nd和Pb同位素组成均表现出印度洋MORB型同位素组成特征;枕状玄武岩(△~(207)Pb/~(204)Pb)_(?)变化范围为9。
3)  Qilian Fold Belt
祁连山造山带
4)  North Qilian Orogenic belt
北祁连造山带
1.
Geochemistry characteristics and palaeogeographic significance of the Ordovician siliceous rocks from Laohushan area,North Qilian orogenic belt;
北祁连造山带老虎山奥陶系硅质岩地球化学特征及古地理意义
2.
From the back-arc basin to foreland basin-Ordovician-Devonian sedimentary basin and tectonic evolution in the North Qilian orogenic belt;
从弧后盆地到前陆盆地——北祁连造山带奥陶纪—泥盆纪的沉积盆地与构造演化
3.
The North Qilian orogenic belt in northwestern China is an elongate tectonic unit situated between the North China plate in the north and the Qaidam plate in the south.
北祁连造山带位于华北板块西南缘,是柴达木微板块与华北板块碰撞形成的加里东造山带。
5)  Qilian-Qinling orogenic belt
祁连-秦岭造山带
6)  East Qilian orogenic belt
祁连造山带东段
补充资料:板带轧制速度规程(见板带轧制规程设计)


板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling

  bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
  
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