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east xinjiang
相关语句
  东疆
    CHARACTERISTICS OF METAMORPHISM IN THE HARLIK METAMORPHIC BELT,EAST XINJIANG,AND ITS TECTONIC ENVIRONMENT
    东疆哈尔里克变质地带变质作用特征及形成构造环境研究
短句来源
    The Lacustrine sediment records of the Environmental changes since the Little Ice Age(LIA) in the northern parts of East xinjiang
    东疆北部地区小冰期环境特征的湖相沉积记录
短句来源
    Method of drainage sediments surveying is applied in geochemical exploration 1∶50 at jiabaishan of East Xinjiang. The sampling den sity is generally 5[(-)0(6)] points per square kilomter,in case of critical anomalyseci ons,8 points per square kilometer.
    东疆夹白山地区1z5万化探普查采用水系沉积物测量的方法,采样密度一般5~6 点/km2,重要区域异常和成矿有利地段采样密度为8 点/ km2. GPS定位,多点组合采样.
短句来源
  东疆
    CHARACTERISTICS OF METAMORPHISM IN THE HARLIK METAMORPHIC BELT,EAST XINJIANG,AND ITS TECTONIC ENVIRONMENT
    东疆哈尔里克变质地带变质作用特征及形成构造环境研究
短句来源
    The Lacustrine sediment records of the Environmental changes since the Little Ice Age(LIA) in the northern parts of East xinjiang
    东疆北部地区小冰期环境特征的湖相沉积记录
短句来源
    Method of drainage sediments surveying is applied in geochemical exploration 1∶50 at jiabaishan of East Xinjiang. The sampling den sity is generally 5[(-)0(6)] points per square kilomter,in case of critical anomalyseci ons,8 points per square kilometer.
    东疆夹白山地区1z5万化探普查采用水系沉积物测量的方法,采样密度一般5~6 点/km2,重要区域异常和成矿有利地段采样密度为8 点/ km2. GPS定位,多点组合采样.
短句来源
  “east xinjiang”译为未确定词的双语例句
    Tectonic Evolution of the Santanghu Basin,East Xinjiang and Its Implication for the Hydrocarbon Accumulation
    新疆东部三塘湖盆地构造演化及其石油地质意义
短句来源
    APPLICATION OF GEOCHMICAL EXPLORATION 1∶50000 IN LOW RELIEF DESERT TERRAINE——AN EXAMPLE OF GEOCHMICAL PROSPECTING AND ANOMALY EXAMINATION FROM JIABAISHAN,EAST XINJIANG
    低山丘陵荒漠景观区1:5万化探方法研究——以东疆夹白山地区化探普查及异常查证为例
短句来源
    REGIONAL DISTRIBUTION PATTERNS OF GEOCHEMICAL DATA IN THE YI-TUN-BU-LA-KE AREA–BE-GE-DA-BAN MOUNTAIN PEAK,EAST XINJIANG KUNLUN MOUNTAINS
    新疆昆仑山布喀达坂峰—依吞布拉克一带岩石地球化学特征及元素分布规律
短句来源
    GEOLOGICAL CHARACTERISTICS AND MINERALIZATION OF HUANG-YANG-LIN ANTIMONY DEPOSIT IN THE EAST XINJIANG KUNLUN AREA
    新疆东昆仑黄羊岭锑矿床地质特征及成矿规律
短句来源
    Zaisan-east Junggar and Kangguer OCeanic basins, Bogda-Harlik and North Mount riftS,andtwelve deep fault 'zones were formed in the north and east Xinjiang.
    寒武纪晚期开始解体,在新疆东、北部形成斋桑-东准噶尔、康古尔两个洋盆,博格达-哈尔力克、北山两个裂谷系和12条深、大断裂带。
短句来源
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  east xinjiang
More than twenty mafic-ultramafic complexes, which host several mediumor large-sized Cu-Ni deposits, occur along the Huangshan-Jingerquan (HJ) belt in East Xinjiang.
      
Geology and genesis of the mafic-ultramafic complexes in the Huangshan-Jingerquan (HJ) belt, East Xinjiang
      


The Meridonal structural zones in western China have been rarely repor- ted,despite their wide distribution. They may be divided into six zones: a)Sichuan-Yunnan—East Qinghai lake zone; b)West Yunnan—West Qinghai lake zone; c)East Tibet—West Gansu zone; d)Central Tibet—East Xinjiang zone; e)Mt.Jolmolungma—Mt.Friendship zone; f)West Tibet—West Xinjiang zone. These zones are characterized by:(a)Presence of large superposed folds and basement faults;(b)Complex mechanical properties,often...

The Meridonal structural zones in western China have been rarely repor- ted,despite their wide distribution. They may be divided into six zones: a)Sichuan-Yunnan—East Qinghai lake zone; b)West Yunnan—West Qinghai lake zone; c)East Tibet—West Gansu zone; d)Central Tibet—East Xinjiang zone; e)Mt.Jolmolungma—Mt.Friendship zone; f)West Tibet—West Xinjiang zone. These zones are characterized by:(a)Presence of large superposed folds and basement faults;(b)Complex mechanical properties,often with the compressive,tensile and shear structural features present in the same stru- ctural zone;(c)A long development and repeated activity,having suffered an E-W compression during the decline of the Latitudinal structural zone; (d)Awider development in central Asia beyond the limits of the western China,and a long,discontinued northward or southward extension. The meridional structural zones in western China are parts of those of the whole earth.They may originate from a change of the rate of the Earth's rotation.

中国西部经向构造体系可划分六个构造带,以4°—5°间距贯穿全区,并向两端延伸,应属全球经向构造体系的组成部分。笔者依据最新地质及地球物理资料,论述了他们的分布特征及其成因机制,并指出它们在地壳演化和寻找有用矿产方面的意义。

The continental block of Xinjiang and its adjacent areas was broken up in the late Cambriantime.Zaisan-east Junggar and Kangguer OCeanic basins, Bogda-Harlik and North Mount riftS,andtwelve deep fault 'zones were formed in the north and east Xinjiang. Since the middle and late Caledonian, the two basins beg3n opening and closins,and three subduction zones, two collision zones andseven island arc belts were formed. At last, the two collision zones were closed up along Karameili andKangguertag...

The continental block of Xinjiang and its adjacent areas was broken up in the late Cambriantime.Zaisan-east Junggar and Kangguer OCeanic basins, Bogda-Harlik and North Mount riftS,andtwelve deep fault 'zones were formed in the north and east Xinjiang. Since the middle and late Caledonian, the two basins beg3n opening and closins,and three subduction zones, two collision zones andseven island arc belts were formed. At last, the two collision zones were closed up along Karameili andKangguertag in middle Variscan. The eastern Xinjiang and its adjacent areas were divided into three paleoplates and ten secondary tectonic elementS, bounded by the colliSion zones, subduction zones anddeep fault zones. After the closins of the two riftS in the late Variscan,the crust was compressed strongly and the tectonic effect within the plate occurred after a series of thrust-nappe structures collided.

显生宙初,新疆曾是一个统一的陆块。寒武纪晚期开始解体,在新疆东、北部形成斋桑-东准噶尔、康古尔两个洋盆,博格达-哈尔力克、北山两个裂谷系和12条深、大断裂带。从加里东中晚期开始,两个洋盆边拉张达消减,形成3条俯冲带、2个对接带和7个岛弧带,最后于华力西中期沿克拉表里、康古尔塔格两个对接带闭合。以对接带、俯冲带和深断裂带为界,将东疆及其邻区划分为西伯利亚、准噶尔和塔里木三大板块,10个次级构造单元。华力西晚期两个裂谷闭合后,中上部地壳强烈水平挤压,产生一系列逆冲-推覆构造等碰撞期后极内构造效应。

Applied the Factor Analysis Method to deal with the spore-pollen and chemical element content data.which obtained from the lacustrine sediment in Balikun Lake,northern parts of east Xinjiang .this paper hasreconstructed the sequence of environmental changes since LIA in Balikun district. The Extensive regionalcomparison show that the results achived in this paper are reliable,so this paper has not only obtained the information of environmental changes since LIA,in Xinjiang from the lacustrine sediment,on...

Applied the Factor Analysis Method to deal with the spore-pollen and chemical element content data.which obtained from the lacustrine sediment in Balikun Lake,northern parts of east Xinjiang .this paper hasreconstructed the sequence of environmental changes since LIA in Balikun district. The Extensive regionalcomparison show that the results achived in this paper are reliable,so this paper has not only obtained the information of environmental changes since LIA,in Xinjiang from the lacustrine sediment,on the other hand,also reclaimed to some extent degree the approaches to deal with the study of environmental changes in aridarea.

本文根据新疆东疆北部巴里坤湖湖相沉积的孢粉及地球化学元素含量分析,运用因子分析法处理数据,恢复了巴里坤地区近500年来的环境演变序列.广泛的区域性对比表明,所获结果具较高可信度,故本文不但获得了在新疆地区由湖相沉积所揭示的小冰期以来的环境演变信息,另一方面丰富了本地区短时代环境演变研究的方法和手段.

 
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