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eastern xinjiang     
相关语句
  新疆东部
     PALEOMAGNETIC STUDY OF THE EASTERN XINJIANG
     新疆东部古地磁研究
短句来源
     STUDY ON ISOTOPIC CHRONOLOGY OF THE MAZHUANGSHAN GOLD MINERALIZATION,EASTERN XINJIANG
     新疆东部马庄山金矿成矿作用同位素年代学研究
短句来源
     Glires of Eastern Xinjiang and Their Zoogeographical Distribution
     新疆东部啮齿动物的分类和分布
短句来源
     Located on the northeastern border of the Tarim Craton in Eastern Xinjiang, Beishan area extends from west to east for about 300 km and from north to south 100 km, in which a series of gold deposits have newly been discovered.
     北山地区位于新疆东部塔里木地块东北缘,东西长约300km,南北宽约100km,近来发现了一系列金矿点。
短句来源
     Zircon SHRIMP U-Pb Age of a Dioritic Pluton in the Harlik Mountain,Eastern Xinjiang, and Its Tectonic Implication
     新疆东部哈尔里克山闪长岩锆石SHRIMP U-Pb定年及其地质意义
短句来源
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  东疆
     Zircon U-Pb Dating of the Rocks from the Harlik Metamorphic Belt in Eastern Xinjiang and Its Geological Significance
     东疆哈尔里克变质带的U-Pb年龄及其地质意义
短句来源
     DISCOVERY OF KB-7 GEOCHEMICAL ANOMALY AND 371-XIBEIPO GOLD-COPPER MINERALIZED ZONE AND IMPLICATIONS IN THE YAXI AREA OF EASTERN XINJIANG
     东疆雅西KB-7化探异常与371-西北坡(金)铜矿化带
短句来源
     Metallogenic background and geochemical characteristics of Lower Carboniferous volcanic rocks in No.371-Xibeipo copper-gold mineralization belt in the Yaxi area,eastern Xinjiang.
     东疆雅西371-西北坡铜金矿化带下石炭统火山岩地球化学特征与成矿背景
短句来源
     Characteristics of Garnets from the Harlik Metamorphic Belt in Eastern Xinjiang
     东疆哈尔里克变质带中石榴子石的特征
短句来源
     Impact and Countermeasure of Local Spring Sandstorm on Environmental Air Quality in Cities of Southern and Eastern Xinjiang
     春季区域性沙尘暴对南疆及东疆城市环境空气质量的影响及应对措施
短句来源
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  新疆东部地区
     AN APPLICATION OF CELL ORE-VALUE PROBABILITY DISTRIBUTION TO APPRAISAL OF IRON RESOURCES IN EASTERN XINJIANG
     单元矿床值概率分布法在新疆东部地区铁矿资源预测中的应用
短句来源
     Analysis of Summer Heavy Rainfall in Eastern Xinjiang
     新疆东部地区夏季暴雨的分析
短句来源
     A PRELIMINARY STUDY ON GEOTECTONICS OF EASTERN XINJIANG
     新疆东部地区大地构造问题探讨
短句来源
     Fauna and Medical Importance of Acarine in Eastern Xinjiang
     新疆东部地区蜱螨区系及医学意义
短句来源
     On the basis of the summer rainfall data of six stations in eastern Xinjiang from 1961 to 2000, NCEP/NCAR 6h reanalysis data and routine observed data, the synoptic and climatic features of the summer heavy rainfall in eastern Xinjiang, along with the circulation patterns, influencing weather systems and their forming mechanism, were investigated, and the physical concept model of the typical case was established, and some premonitory signs for the genesis of heavy rainfall were presented.
     利用1961—2000年共40年新疆东部地区6站夏季降雨量资料、NCEP1°×1°的6小时再分析资料和常规探测等资料,对我国新疆东部地区夏季暴雨的天气气候特征、环流形势、影响天气系统及其暴雨形成的机制进行分析研究,并给出典型个例清晰的物理概念模型,提供了有参考意义的前兆依据。
短句来源
  新疆哈密
     DISCOVERY AND CHARACTERISTICS OF CU-RICH STELLERITE IN SANCHAKOU COPPER DEPOSIT,EASTERN XINJIANG
     富铜红辉沸石在新疆哈密三岔口铜矿床的发现与矿物学特征
短句来源

 

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      eastern xinjiang
    Study on chronology and origin of the mazhuangshan gold deposit in Eastern Xinjiang
          
    Chronology and origin of the Jinwozi gold deposit in Eastern Xinjiang
          
    The East Tianshan is a remote Gobi area located in eastern Xinjiang, northwestern China.
          


    By using the method of cluster analysis, the annual variation curve types of the sunshine percentage in China are divided into 12 divisions. The basic types are: the Southern region which has low sunshine percentage but with sunny and dry summer causing an inverted 'V' variation; northeast China, north China and southwest China which has more sunshine but with summer rain; the three sunny regions are: the Southern Xinjiang, the Eastern Xinjiang and the Northern Xinjiang, and the South China...

    By using the method of cluster analysis, the annual variation curve types of the sunshine percentage in China are divided into 12 divisions. The basic types are: the Southern region which has low sunshine percentage but with sunny and dry summer causing an inverted 'V' variation; northeast China, north China and southwest China which has more sunshine but with summer rain; the three sunny regions are: the Southern Xinjiang, the Eastern Xinjiang and the Northern Xinjiang, and the South China Sea region. There are five transition regions, and another region located between the Southern region and the South China Sea region.

    本文根据日照百分率年变程曲线类型,应用聚类分析方法,把全国划分为12个日照区。主要类型有:冬半年少日照但盛夏干旱多日照形成“A”型的南方区;冬半年多日照但盛夏多雨少日照形成“V”型的东北—华北—西南区;全年日照丰富的南疆区,北疆区和东疆区;以及属于热带干湿季比较分明的南海区。另外,在南方区和东北—华北—西南区之间有5个过渡区;在南海区和南方区之间也有1个过渡区。这12个日照区的地域分布及日照百分率年变程曲线类型与我国天气气候特点很吻合。

    Early Palaeozoic crust types of Gansu-Menggu Beishan area and Eastern Xinjiang Tianshan Mts. have been researched and divided into old continental crust,early Palaeozoic ocean crust,tensile transtion-al crust, convergent transtional crust. At early Palaeozoic, along the line Kumishi-Kawabulake-Xing-xingxia Xiaohuangshan, it splited from east to west since late Sinian Period. The whole open was at late Cambrian to early Ordovician &formed Kumishi- Xiaohuangshan ocean basin. The micro- continent of Middle...

    Early Palaeozoic crust types of Gansu-Menggu Beishan area and Eastern Xinjiang Tianshan Mts. have been researched and divided into old continental crust,early Palaeozoic ocean crust,tensile transtion-al crust, convergent transtional crust. At early Palaeozoic, along the line Kumishi-Kawabulake-Xing-xingxia Xiaohuangshan, it splited from east to west since late Sinian Period. The whole open was at late Cambrian to early Ordovician &formed Kumishi- Xiaohuangshan ocean basin. The micro- continent of Middle Tianshan Mts. separated from the north of Tarim old plate on the northern. The Qieme fault zone played a important role in control transform fault of both side east and west tectonic development. The crust types of Gansu-Menggu Beishan are more complicated than Eastern Xinjiang Tianshan' s. There were Ordovician tensile transitional crust-rift zone and Silurian convergent transitional crust-trench-arc-basin system from early to late. During Later Palaeozoic Era, whole area tectonic evolution entered open and closed alternatively period,tensile transtional crust formed at the open period. At Early Palaeozoic, ocean has existed untill Devonian-Carboniferous at the Hazibulaketage region of the northern Kuluke-tage.

    本文研究了甘蒙北山及东疆天山早古生代地壳类型,划分为元古代的古陆壳、早古生代洋壳、拉张型过渡壳、汇聚型过渡壳。早古生代沿着库米什—卡瓦布拉克—星星峡—小黄山一线自震旦世晚期由东向西逐渐开裂,于晚寒武世至早奥陶世全面打开,形成库米什—小黄山洋盆。其北侧由塔里木古板块北缘分离出中天山微大陆。且末断裂带斜贯全区,起了控制东西两侧构造发展的转换断层作用。甘蒙北山较东疆天山的地壳类型更为复杂,先后发育有奥陶纪拉张型过渡壳—裂谷带和志留纪汇聚型过渡壳—沟弧盆体系。晚古生代全区构造演化进入开合交替时期,其开时形成拉张过渡壳,早古生代洋区在库鲁克塔格北缘哈孜布拉克塔格地区延续到泥盆—石炭纪。

    The geological and geophyscal data have proved that Kangguertage fault zone is an impor-tant fault zone in the eastern Xinjiang. It is not a plate subducted zone but is only a terrane boundaryfault zone. It's evolutional history can be divided into three main phases: deep fracture action, ductileShear deformation and fault block action. It controls not only the formation and development of Aqis-han-Huangshan composite terrane, but also directly the distribution and shape feature of the Cu-Ni orebearing...

    The geological and geophyscal data have proved that Kangguertage fault zone is an impor-tant fault zone in the eastern Xinjiang. It is not a plate subducted zone but is only a terrane boundaryfault zone. It's evolutional history can be divided into three main phases: deep fracture action, ductileShear deformation and fault block action. It controls not only the formation and development of Aqis-han-Huangshan composite terrane, but also directly the distribution and shape feature of the Cu-Ni orebearing mafic-ultramafic complex in Huangshan-Jingerquan area.

    新疆东部的康古尔塔格断裂带不是板块俯冲带,而是地体的一条边界断裂带。其演化历史可分为三个主要阶段:深断裂活动阶段、韧性剪切活动阶段和断块活动阶段,并相应控制了阿齐山-黄山复合地体的形成与发展,还直接控制了黄山-镜儿泉地区铜镍含矿镁铁超镁铁杂岩体的空间展布与形态特征。

     
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