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east kunlun mountain
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  东昆仑
     Mineralogical Features of Kendekeke Gold-Nonferrous Metal Deposit in East Kunlun Mountain,Qinghai Province
     青海东昆仑肯德可克金—有色金属矿床矿物特征研究
短句来源
     The gold deposits, having been found in the middle belt of east Kunlun mountain, are the cryptoexplosive breccia, skarn, altered rock and quartz vein.
     东昆仑中带 ,发现和查明和金矿有蚀变构造岩型、隐爆角砾岩型、矽卡岩型和石英脉型 4种矿化类型 ,其中前两者为金的主要成矿类型。
短句来源
     The cobalt deposit types in east part of East Kunlun mountain mainly include spout deposition type and skarn type etc.
     东昆仑东段的钴矿床类型主要有喷流沉积型、矽卡岩型等。
短句来源
     A STUDY OF THE REGIONAL METALLOGENETIC REGULARITY IN EAST KUNLUN MOUNTAIN
     东昆仑区域成矿规律初步研究
短句来源
     The petrogenetic characteristics of Heishangou Group and Haerzha Group of late Devonian in east Kunlun Mountain are similar to those of Yak Group, as they consist of clastic rocks of terrigenous facies and littoral shallow sea facies, in addition to carbonatite, intermediate-acidic volcanic assemblage, and belong to typical molasse formation in a stretch-rift system, which is indicative of the beginning of basin evolvement in the late Paleozoic stretch-rift system.
     东昆仑晚泥盆世黑山沟组和哈尔扎组岩性组合特征与牦牛山组极为相似,均为一套陆相、滨浅海相的碎屑岩、碳酸盐岩和中酸性火山岩组合,为典型的裂陷伸展型磨拉石建造,是晚古生代裂陷伸展盆地演化开始的标志。
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  东昆仑山
     Gold-Search Prospects in Southern Slope of Western Part of East Kunlun Mountain and in Kekexili Area
     东昆仑山西段南坡及可可西里地区找金前景简介
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  “east kunlun mountain”译为未确定词的双语例句
     and ② there are 70 kaBP terraces in the Central Kunlun Mountains and 50 kaBP terraces in the East Kunlun Mountain, and their formation in the eastern and western parts of the Kunlun Mountains in the two stages was not synchronous.
     ②昆仑山中部地区具有70kaBP的阶地,昆仑山东部地区具有50kaBP的阶地,这2个时期昆仑山东西部河流、湖岸地貌的形成不具有同步性。
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This paper expounded the tectonic problems in AQK area (the Altyn, Qilian and east Kunlun Mountain area) by analysing and contrasting all the"constructive"and "des-tructive"events as well as by structural sieving. The tectonic development of the Alt-ynQilianshan and E. Kunlun fold belt shows that they are not independent fold belts, in the early period they didn't form independent structural systems,and they were components of Kunlun-Qinling latitudinal tectjnic system. Their present winding...

This paper expounded the tectonic problems in AQK area (the Altyn, Qilian and east Kunlun Mountain area) by analysing and contrasting all the"constructive"and "des-tructive"events as well as by structural sieving. The tectonic development of the Alt-ynQilianshan and E. Kunlun fold belt shows that they are not independent fold belts, in the early period they didn't form independent structural systems,and they were components of Kunlun-Qinling latitudinal tectjnic system. Their present winding forms were the result of migration of crustal segments .According to the theory of formation of the latitudinal tectonic system, they were situated originally at where occu-ppied now by the E.Kunlun mountain.The formula of the spherical harmonic function delineates the occurrence of latitudinal tectonic systems at given latitudes of the earth, but the latitudinal tectonic systems do not always keep in the E-W direction and equidistances. Most of them were formed very early in earth history and were liable to change in later crustal development.The Kunlun-Qinling latitudinal system is just one of the example showing how the dextral rotation of QinghaiXizang land mass had deflected the E-W tectonic zone. Of course, the force which made Qinghai-Xizang land mass rotate was coming from the inertia force of the earth's rotation.

纬向构造带产生的特定纬度带,是其构造“发生床”,在这些带上产生的构造形体(包括阶段性的全部建造和改造)是其构造“成生体”。纬向构造带有长期活动、多阶段发展的特点,其不同阶段促成不同的构造成生体。阿祁昆地区弯转多姿的构造带是秦昆系的古老成生体迁移扭变的结果,扭变的主因是青藏地块的右旋转动。

The Upper Triassic series distribute not only along the south margin of east Kunlun Mountain but also of west Kun-lun Mountain, They are composed of epizonal metamorphic flysch sediments at Quanshuigou area. To the north-west they arehypometamorphic rocks and migmatite granites at Fulugou area. The varietis in metamorphism, mechanism of deformation andstructural atyle represent different tectonic levels formed in different depth. The structures at Quanshuigou area are formed be-low the frontal surface...

The Upper Triassic series distribute not only along the south margin of east Kunlun Mountain but also of west Kun-lun Mountain, They are composed of epizonal metamorphic flysch sediments at Quanshuigou area. To the north-west they arehypometamorphic rocks and migmatite granites at Fulugou area. The varietis in metamorphism, mechanism of deformation andstructural atyle represent different tectonic levels formed in different depth. The structures at Quanshuigou area are formed be-low the frontal surface of cleavage and that at Fulugou area are below the upper limit of schistoity.

西昆仑山南侧沿北西向分布的变质复理石海相碎屑岩系,其时代主要属晚三叠世,是巴颜喀喇山群的西延部分。它的东段和西段岩石变质程度、构造样式和变形机制的不同,是同一构造带中不同构造层次构造的反映。东段属下部构造层次,西段属深部构造层次和深熔花岗岩。它们形成于晚三叠世昆仑地块南缘的陆缘盆地,印支期褶皱变质,燕山期和喜山期的挤压、抬升和剥蚀,使东西两段出露了于不同深度构造层次形成的构造。

As an independent hydrological unit, Hexi-Alashan Region of the northwestern China is an area of more than 500000 square kilometers and contains principally three separated inland river systems, namely, Shule River, Ruoshui River anl Shiyang River. There are fishes of 12 species/subspecies, 4 genera and 2 families (Cobitididae and Cyprinidae) naturally distributed in the region and 7 in 12 are endemio. Ten species of scaleless noemacheilini fishes and Gymnocyprinus eckloni chilianensis characterize the features...

As an independent hydrological unit, Hexi-Alashan Region of the northwestern China is an area of more than 500000 square kilometers and contains principally three separated inland river systems, namely, Shule River, Ruoshui River anl Shiyang River. There are fishes of 12 species/subspecies, 4 genera and 2 families (Cobitididae and Cyprinidae) naturally distributed in the region and 7 in 12 are endemio. Ten species of scaleless noemacheilini fishes and Gymnocyprinus eckloni chilianensis characterize the features of fish-fauna of the region shared with Qinghai-Tibet Plateau or High Central Asia: simpler faunal components, fishes Schizothoracinae and scaleless Noemacheilinae in dominant position rare pedatory fishes, specialized to adapt to the harsh conditions of water bodies with high altitude and low temperature, and fish taxa differentiated due to local and limited distribution. The distribution of Carassius auratus in the region is a feature of the region's position at the margin of Qinghai-Tibet Plateau and the border of the arid inland region of Central Asia. The fish distribution also displays horizental and vertical geographical differences in the region.In phenetic overall similarities, the descrimination and the cluster analysis of average faunal resemblance (AFR) indicate these three river systems male up an independent ichthyogeographical unit, with Ruoshui River as its center and most closely related to Qaidam Basin faunally. PAE and PAUP give two area cladograms basically consistent and, basing on the vicariance theory, reveal the fish geographical relationships as following: Shule River and Ruoshui River, they and Shiyang River, Hexi Area and Qaidam (as well as Hequ, i.d., the Upper Huang He River), anl all of them and Kuku Nut Lake are a series of sister area groups, or in other words, they are all in a large monophyletic area group. While Longzhong and Hetao, and they and Inner Mongolia Plateau are also sister area groups and all of them make up other large monophyletic area group. Then these two large area groups are sister area groups and make up a monophyletic area group at a higher level.Furthermore, the evolutionary history of the fish fauna of Hexi-Alashan Region is recounted in the light of the phylogeny of the fishes and the data of the geological history of the area. It is elucidated that mainly the tectonic movements, especially the Himalaya Movement, and the climatic changes since Tritary Period have resulted in the area vicariance of HexiAlashan Region and the isolation of the river systems, the long-termed isolation has caused the differentiation of the fish taxa and thus the modern pattern of fishes distribution is determined in this region.Then the problem of the zoogeographical division is considered for the fresh-water fishes distributed in the Northwest and Hequ-Qilian Province is suggested to enlarge and replace Maqu Province, which is situated in the northeastern part of Qinghai-Tibet Plateau, to the north of Bayan Khara Mountains and East Kunlun Mountains, including four sub-divisions (Biogeographical Prefectures) Hexi-Alashan, Qaidam, Hequ, and Kuku Nur Lake, and suboradinating to High Central Asia Region or he Northwest Plateau or West China Region. Finally, it is pointed that the approach PAE is one merit to be applied to the research on biogeographical problems in China.

中国西北河西阿拉善内流区,主要含石羊河、弱水、疏勒河三个分离的内陆水系,为一独立的水文单元,面积逾50万平方公里,天然分布了鲤科2属2种、鳅科条鳅亚科2属10种。组成鱼类区系的这12个土著种中,有7种/亚种为本区特有。10种无鳞条鳅和河西花斑裸鲤表征了本区和中亚山地及青藏高原的共同鱼类区系特征:区系组成简单,裂腹鱼类和无鳞条鳅类占优势,很少凶猛种类,适应高寒水体严酷环境的种类特化,和局限分布的类群分化。鲫的存在体现了本区处在青藏高原和中亚内陆干旱区边缘的特点。这些鱼类在本区也表现出水平和垂直分布的差异。 平均动物区系类似性(AFR)判别和数值聚类分析,从表相学全面相似性上阐明,本区三水系形成以弱水为中心的独立鱼类地理学单位,与柴达木盆地的区系关系最密切。特有性俭吝分析(PAE)和俭吝性种系发生分析(PAUP)产生了基本一致的区域支序图,从分替论的鱼类地理亲缘上揭示了:疏勒河与弱水,它们与石羊河,河西与柴达木(和河曲区即黄河上游),它们与青海湖是一系列姐妹群关系,一起组成一个大的区域单系群;而陇中与河套,它们与内蒙古高原,又依次为姐妹群关系,一起组成另一大的单系群;两大单系群作为姐妹群,形成更高一级区域单系群。...

中国西北河西阿拉善内流区,主要含石羊河、弱水、疏勒河三个分离的内陆水系,为一独立的水文单元,面积逾50万平方公里,天然分布了鲤科2属2种、鳅科条鳅亚科2属10种。组成鱼类区系的这12个土著种中,有7种/亚种为本区特有。10种无鳞条鳅和河西花斑裸鲤表征了本区和中亚山地及青藏高原的共同鱼类区系特征:区系组成简单,裂腹鱼类和无鳞条鳅类占优势,很少凶猛种类,适应高寒水体严酷环境的种类特化,和局限分布的类群分化。鲫的存在体现了本区处在青藏高原和中亚内陆干旱区边缘的特点。这些鱼类在本区也表现出水平和垂直分布的差异。 平均动物区系类似性(AFR)判别和数值聚类分析,从表相学全面相似性上阐明,本区三水系形成以弱水为中心的独立鱼类地理学单位,与柴达木盆地的区系关系最密切。特有性俭吝分析(PAE)和俭吝性种系发生分析(PAUP)产生了基本一致的区域支序图,从分替论的鱼类地理亲缘上揭示了:疏勒河与弱水,它们与石羊河,河西与柴达木(和河曲区即黄河上游),它们与青海湖是一系列姐妹群关系,一起组成一个大的区域单系群;而陇中与河套,它们与内蒙古高原,又依次为姐妹群关系,一起组成另一大的单系群;两大单系群作为姐妹群,形成更高一级区域单系群。 进而结合有关的鱼类种系发生和区域地质历史资料,叙述了河西

 
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