1) 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
2) Northern Qilian Mountains
北祁连山
1.
Magmagenesis of Ordovician back-arc basins in the Northern Qilian Mountains;
北祁连山奥陶纪弧后盆地火山岩浆成因
2.
Discusses metallogenic feature of Shijuligou copper-rich ore deposits in Northern Qilian Mountains.
讨论北祁连山石居里沟富铜矿床成矿特征 ,通过分析认为 :成矿环境为中奥陶世弧后扩张脊 ;容矿岩石为蛇绿岩套上部火山岩或火山—沉积岩系 ;矿体赋存部位受海底裂隙系统的控制 ;含矿热液起源于海水与玄武岩在高温下的反应 ,成矿金属元素主要来自火山岩 ,矿化剂硫来自二者。
3.
The west sector of the northern Qilian Mountains is well-known for the Jingtieshan type iron deposits.
北祁连山西段以产镜铁山式铁矿而著称,近几年找金和找铜又有新突破。
3) North Qilian Mountain
北祁连山
1.
Geology and Geochemistry of Volcanic Rocks of the Early Ordovician Yingou Group in the Western Part of North Qilian Mountain and Their Tectonic Setting;
北祁连山西段早奥陶世阴沟群火山岩的构造背景
2.
Recent discovered Hanshan gold deposit is a structure-controlled altered rock type related with intrusive rocks in North Qilian Mountain.
寒山大型金矿是近年来在北祁连山西段发现的与基性火山岩有关的构造蚀变岩型金矿。
3.
In the past several years,more than a dozen of gold deposits and gold occurrences,such as Hanshan,Yingzuishan,Changma,Hongkouzi and Zhulong,have been discovered in the western part of North Qilian Mountain.
北祁连山西段金矿床以剪切带型为主 ,控矿的主导因素是剪切构造和成矿流体。
4) the North Qilian mountains
北祁连山
1.
The characteristics,mineralization and prospecting indi- cations of Cyprus-type copper deposits in mid-west section of the North Qilian mountains,China;
北祁连山中西段塞浦路斯型铜矿特征、成矿作用及找矿标志
2.
A complete progressive and regressive cycle occurred in the early Early Carboniferous in the eastern part of the North Qilian Mountains.
北祁连山东部早石炭世早期经历了一次完整的海水进退旋回。
3.
The adakite belt in the eastern section of the North Qilian Mountains was derived from the partial melting of the northwards subducted oceanic crust of the Laohushan back-arc basin.
北祁连山东段存在一条埃达克岩条带,由向北俯冲的老虎山弧后盆地洋壳部分熔融形成,其形成过程具有高温、高压、富含挥发分流体、高氧逸度和快速上升的特点,有利于Cu、Au等成矿物质在埃达克岩中富集。
5) northern of Qilian mountains
祁连山北坡
1.
The text opening out the continuance climate warming is the essence characteristic of northern of Qilian mountains.
本文揭示了气候持续变暖是祁连山北坡现代气候变化的基本特征。
6) northern slope of Qilian Mountains
祁连山北坡
1.
Investigating the rodent population on northern slope of Qilian Mountains, 2 order 6 family 14 genus 23 species of rodent animals were found and the diversity of rodent animal population reduced with rising of elevation.
对祁连山北坡啮齿动物种群调查,共发现啮齿动物2目6科14属23种,啮齿动物种群多样性随海拔的升高而降低,并提出了该地的主要鼠害种类及控制建议。
补充资料：祁连山
祁连山
Qilian Shan
QiliQn Shan祁连山(Qilian shan)中国青藏高原东北边缘山脉。匈奴语呼天为“祁连”，故名。位于青海、甘肃两省交界处。西起当金山口与阿尔金山山刀永相接，东至黄河谷地与秦岭、六盘山相连，南抱柴达木、共和盆地，北临河西走廊。亦称走廊南山。东西长达1 000千米，南北宽200一300千米，面积20.6万平方千米。由一系列西北一东南走向的平行山脉和山间谷地组成。地势西北高、东南低，北坡陡峻，南坡和缓。山峰海拔多在4 000米以上，最高峰为疏勒南山团结峰(又名宰吾结勒)，海拔5 808米。山体多由石灰岩、花岗岩组成。海拔4 500米以上的山峰终年积雪，冰川广布。祁连山由西向东分为三段。 西段为疏勒河上游谷地以西。自北至南有照壁山、大雪山(野马山)、野马南山、党河南山、察汗鄂博图岭、土尔根达板和柴达木l一日。山势高峻，海拔多在3 500~5 000米之间，主峰大雪山海拔5 483米。大部山坡植被稀疏，阴坡生长小片针叶林及灌木林。发源西段的疏勒河、党河，流人河西走廊。位于阿尔金山脉和祁连{妇交接处的当金山口是重要隘口，海拔3 649米，南北长约27千米，谷狭路隘，两侧山峦重迭，奇峰陡立，地势险要。柳园一格尔木公路从山口通过，是沟通河西走廊和柴达木盆地间的重要通道。距嘉峪关市81千米的镜铁山铁矿一，储量大，全国闻名。 中段为疏勒河上游谷地至扁都口。由北向南有走廊南山、托来山、托来南山、疏勒南山、哈拉南山、宗务隆山、青海南山，其间夹有黑河谷地、青海湖盆地。主峰祁连山海拔5 547米。阴坡峡谷，林木茂密，生长云杉林及冷杉林，海拔4 000米以上植被稀少。北麓水源丰富。共有大小河流12条，其中黑河最大。南麓干燥，植被稀少。由西北向东南有近28个沟口，北距甘肃省民乐县28千米处的扁都口最为重要，是西宁一张掖公路之咽喉。扁都沟贯通南北，沟长32千米，谷宽仅30一200米，海拔3 200-4 150米。两侧山峰连绵起伏，多为悬崖绝壁，山坡灌木丛生，童子坝河沿沟北流。山间溪多流长，水质良好。有西宁一嘉峪关的公路经扁都口斜穿山地，是青海和一甘肃间又一通道。 东段为扁都口以东。自北向南有冷龙岭、乌稍岭、大通山、拉脊山等，海拔2 400一3 500米。冷龙岭最高，海拔4 843米。海拔3 000米的阴坡、谷底，为茂密的森林和草原;3 200一4 000米为高山草原草甸及灌木林。阳坡均为山地草原。大通河由西向东流，河谷地势低平。盐矿资源丰富。青海湖为中国最大咸水湖泊，周围为良好草场，是发展畜牧业的理想地区。煤矿储量丰富，著名的有木里一江仓煤矿和九条岭煤矿。有兰州一乌鲁木齐铁路、公路南北纵穿。 西段为高寒大!淤哇干旱区，中段和东段为高寒大陆性半干旱区，1月平均气温一16-一10℃，7月平均气温9一16℃。东段夏季雨水较多，中段为湿润干燥过渡区，雨量渐少，西段极端干燥。最大冻土深1.5一2.0米。祁连山山体庞大，山势险峻，为河西走廊的重要依托。(张立学)祁连山一瞥 孟昭瑞摄
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