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east kunlun mountains     
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  东昆仑
     Ar-Ar dating of orogenic gold deposits in northern margin of Qaidam and East Kunlun Mountains and its geological significance
     柴北缘—东昆仑地区造山型金矿床的Ar-Ar测年及其地质意义
短句来源
     The unroofing of the upper 3km rocks in the East Kunlun Mountains lasted about 45 Ma at least, but only 2~5 Ma in some part of the West Kunlun Mountains.
     在剥蚀程度上,东昆仑最上部3km的去顶至少延续了45Ma,而西昆仑公格尔—塔什库尔干地貌单元只延续了2~5Ma。
短句来源
     The overthrusting in the southern East Kunlun Mountains occurred in the late Oligocene-early Miocene, mainly at 26-13.5 Ma.
     东昆仑南部逆冲推覆构造的发育时代为渐新世晚期—中新世早期,主要形成、活动时期为26~13.5Ma;
短句来源
     Geochemical Characteristics and Tectonic Setting of the Early Carboniferous Volcanic Rocks in East Kunlun Mountains
     东昆仑早石炭世火山岩的地球化学特征及其构造背景
短句来源
     PRIMARY DISPERSION HALO AND ITS MODEL IN Ⅲ ORE SEGMENT OF WULONGGOU GOLD DEPOSIT, EAST KUNLUN MOUNTAINS
     东昆仑五龙沟金矿床Ⅲ矿段原生晕特征及模式
短句来源
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  东昆仑山
     PLACER GOLD AND ITS ORIGIN IN WESTERN SECTION OF EAST KUNLUN MOUNTAINS,XINJIANG
     新疆东昆仑山西段砂金矿特征及成因探讨
短句来源
     A Large Transpression Zone at the South Margin of the East Kunlun Mountains and Oblique Subduction
     东昆仑山南缘大型转换挤压构造带和斜向俯冲作用
短句来源
     The general structure of the basin is marked by the tectonic framework of compressional ramp of the East Kunlun Mountains and the Qilian Mountains toward and subsidence of the central part of the basin.
     盆地的总体结构表现为东昆仑山和祁连山相向向盆地挤压对冲,盆地中部沉降的构造格局。
短句来源
     Geological features and origin of the Baigan Lake W-Sn deposit in the Ruoqiang area, East Kunlun Mountains, China.
     东昆仑山若羌地区白干湖钨锡矿床地质特征及成因
短句来源
     POLYGONAL RULE FOR ASSESSING THE DISCORDANT U-Pb DATA OF SINGLE-GRAIN ZIRCON BY TIMS∶TAKING HIGH-GRADE METAMORPHIC ROCKS FROM DABIE AND EAST KUNLUN MOUNTAINS AS EXAMPLES
     热离子质谱测定的颗粒级锆石U-Pb不一致年龄数据处理的多边形准则——以大别山和东昆仑山深变质岩为例
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  东昆仑地区
     Ar-Ar dating of orogenic gold deposits in northern margin of Qaidam and East Kunlun Mountains and its geological significance
     柴北缘—东昆仑地区造山型金矿床的Ar-Ar测年及其地质意义
短句来源
     Wulonggou gold deposit in Dulan county, Qinghai province is the most important one in East Kunlun Mountains. The study on its minerogenetic mechanism and conditions is very important.
     青海省都兰县五龙沟金矿床是青海省及东昆仑地区一个十分重要的金矿床 ,其成矿条件及成矿作用的研究对工作程度很低的东昆仑地区金矿找矿工作具有十分重要的意义。
短句来源
     Katelixi copper zinc deposit is the type of marine volcanic sediment sulfide deposit first discovered in east Kunlun Mountains, and its formation is controlled by the volcanic rocks of Tuokuzidaban Group in Carboniferous. The host rocks for the ores are gray-green tuff intercalated in limestone and siltstones occurring in layers or lens.
     卡特里西铜锌多金属矿是新疆东昆仑地区首次发现的海相火山沉积型硫化物矿床,该矿产于下石炭统托库孜达坂群内的火山岩地层中,矿体分布明显受地层控制,含矿岩性为一套双峰式火山岩上部的灰绿色基性凝灰岩,一般呈平行层状、似层状、透镜状夹于灰岩中及灰岩与含炭粉砂岩的接触处。
短句来源
  东昆仑南缘
     The convergence boundary between the East Kunlun terrane and the Bayan Har-Songpan Garze terrane of the Northern Tibet plateau is a large transpressional zone at the south margin of the East Kunlun Mountains.
     东昆仑地体和巴颜喀拉—松潘甘孜地体之间的会聚边界是一条位于东昆仑南缘的大型转换挤压构造带。
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      east kunlun mountains
    The Tieshidas Group in Qimantag, a branch of the East Kunlun Mountains, was classically considered the Caledonian basement, and classified into Middle-Upper Ordovician, Upper Ordovician or simply Lower Paleozoic.
          


    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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