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1)  North Qilian metallogenic belt
北祁连成矿带
2)  Qilian metallogenic zone
祁连成矿带
1.
On the basis of a synthetic analysis of ore-forming conditions and regional mineralization characteristics in the Qilian metallogenic zone, it is proposed that marine volcanic, contact metasomatic (skarn), meta-sedimentary (including sedimentary exhalative) and ductile shear zone types are the major target ore-deposits in the zone.
通过对祁连成矿带地质、矿产、物探、化探、遥感等资料的综合分析,并结合野外调研和室内的再研究,共圈定69处成矿远景区,其中A类5处,B类23处、C类41处。
3)  W materials ore band of Qilian area
祁连钨多金属成矿带
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)  Northern Qilianshan fault zone
北祁连山断裂带
6)  North Qilian mountains
北祁连山
1.
SHRIMP U-Pb Geochronological Research on Detrital Zircons from the Beidahe Complex-Group in the Western Segment of the North Qilian Mountains, Northwest China;
北祁连山西段北大河岩群碎屑锆石SHRIMP U-Pb年代学研究
2.
Reconstruction of protoliths of metamorphic rocks and tectonic setting of the Haiyuan Group in the Haiyuan in the eastern segment of the North Qilian Mountains, China.;
北祁连山东段海原一带海原群变质岩原岩恢复及其构造背景
3.
Chronology and Geological Significance of Chelugou Dacite Porphyry in North Qilian Mountains;
北祁连山车路沟英安斑岩的年代学及地质意义
补充资料:成矿分带
成矿分带
metallogenic zone 

   在含矿流体的活动过程中,由于地质因素和物理化学条件的变化,导致不同的矿石依次产出,形成不同矿石组合的带状分布。例如,在沉积铁矿床中,常表现出不同的矿石相沿沉积当时的海岸作带状分布,距岸由近到远的成矿分带为:①氧化物带(赤铁矿);②硅酸盐带(鲕绿泥石);③碳酸盐带(菱铁矿);④硫化物带(黄铁矿)。又如在气化热液矿床中,含矿气液随着离热源距离的增大,以及物理化学条件的变化,不同矿物的沉淀常依次成带状。例如,中国湖南柿竹园矿床中,自含矿花岗岩体向外,或由深处向浅处,可分出钨带→锡带→铋带→铜带→锌带→铅带。
   成矿分带按其空间产出情况,有水平分带和垂直分带;按其规模大小,有区域成矿分带、矿床分带和矿体分带。区域成矿分带受多种因素控制,如中国江西南部为钨矿带,北部为铜(金)矿带,这是因为两地的构造背景、岩浆岩类型及变质岩基底等有明显差异造成的。
   成矿分带反映了成矿作用在空间上的变化规律,查明这种带状分布规律,对指导矿产勘查和矿山开发均有实际意义。
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