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塔里木陆块
相关语句
  tarim land plate
     Tarim land plate and Kazakhstan plate was divided by north Tarim ophiolite belt;
     以塔里木北缘蛇绿岩带为界,将塔里木陆块与哈萨克斯坦板块分开;
短句来源
     Tarim land plate and Caucasia - Qiangtang plate was divided by Kangxiwa ophiolite belt formed by multi-period subduction.
     以多期俯冲形成的康西瓦蛇绿岩带将塔里木陆块与高加索—羌塘板块分开.
短句来源
  “塔里木陆块”译为未确定词的双语例句
     Each tec-tonic evolution stage within Talimu Basin results from tectonized events around Talimu Basin,and each tectonic movement controls the style of sedimentary basin and the changes of basin properties in Talimu craton.
     每次构造演化都与其周边的构造活动事件密切相关,从而控制了塔里木陆块内的沉积盆地样式及盆地属性的演化。
短句来源
     Wunan gold deposit is located in the active zone of northern margin of Tarimu plate, which concretely exist in the structure unit of triphibian edge in the late Paleozoic in southern Tianshan.
     梧南金矿床位于塔里木陆块北缘活动带,属南天山晚古生代陆缘构造单元。
短句来源
     Most of Pb-Zn deposits are located in 3 important mineralized belts: the south margin of Altai Mountains, the middle Tianshan Mountain and west margin of the Tarim Basin. The south margin of Altai Mountains and west margin of Tarim Basin are the most important deposit areas in Xinjiang.
     铅锌矿床主要分布在阿尔泰山南缘、中天山和塔里木陆块(盆地)西缘3条重要成矿带上,特别是阿尔泰南缘和塔里木陆块西缘是新疆大中型铅锌矿床最重要的2个集中分布区.
短句来源
     Based on the tracing of multi-isotopes as Sm, Nd, Rb, Srand Pb, it is presented that Alashan block is a micro-landmass relative to theDaxing'anling-Mongolian Orogen belt but not the past being part of the North Chinaplaeocontinent or relative to Tarim plaeocontinent. Afterwards, Two II class, Four IIIclass and eight IV class structure units were sorted out.
     依据Sm、Nd、Rb、Sr、Pb等多元同位素示踪,提出阿拉善地块整体上可能为亲兴蒙造山带微陆群的微陆块,而不是过去认为的属华北陆块或亲塔里木陆块
短句来源
     Qimantage terrestrial volcanics: petrologic evidence of active continental margin of Tarim Plate during late Indo-China epoch.
     祁漫塔格陆相火山岩:塔里木陆块南缘印支期活动大陆边缘的岩石学证据
短句来源
更多       
  相似匹配句对
     S TUDY ON PALAEOMAGNETISM OF TARIM CRATON SINCE LATE PALAEOZOIC
     塔里木陆块晚古生代以来古地磁特征研究
短句来源
     Resurgence of the Tarim River
     塔里木河的复活
短句来源
     THE AGE DETERMINATION OF DYKES IN THE BACHU-KEPING REGION OF THE TARIM CRATON
     塔里木陆块巴楚—柯坪地区脉岩时代的古地磁研究
短句来源
     An Investigation of Ectoparasite on Lepus yarkandensis
     塔里木兔体外寄生物的调查研究
短句来源
     5) West Shandong island arc TTG complex greenstone belts(2.70~2.60Ga);
     5 )胶辽陆块 ;
短句来源
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The Tarim Craton is one of three main cratons of China. Its developmental history and tectonic evolution are very interesting to geologians. Study on the ploblems is very useful not only to approach of structural framework and developmental history of the earth but also to study on formation of some mineral resources and ore-controlling tectonic system.

塔里木陆块晚古生代以来极移曲线具有相似的规律,二叠纪以来塔里木陆块是一个稳定的整体.经统计各时代古地磁极位置:晚石炭世:184.9°,56.0°N;二叠纪:194.4°,64.4°N;三叠纪:206.0°,78.2°N;侏罗纪:251.6°,75.9°N;白垩纪:296.3°,75.8°N;老第三纪:223.4°,75.3°N;新第三纪:268.3°,79.9°N.

Talimu Basin has experienced polyperiod tectonic evolution from pre -Sinian to Car-bonifeous.Four stages are divided:(1)basement consolidation during pre-Sinian;(2)intracraton depression;aulacogen and passive continental margin from Sinian to Ordovician;(3)margin rise of the craton from Silurian to Devonian;(4)Intracraton depression during Carbonifeous.Each tec-tonic evolution stage within Talimu Basin results from tectonized events around Talimu Basin,and each tectonic movement controls the style of sedimentary...

Talimu Basin has experienced polyperiod tectonic evolution from pre -Sinian to Car-bonifeous.Four stages are divided:(1)basement consolidation during pre-Sinian;(2)intracraton depression;aulacogen and passive continental margin from Sinian to Ordovician;(3)margin rise of the craton from Silurian to Devonian;(4)Intracraton depression during Carbonifeous.Each tec-tonic evolution stage within Talimu Basin results from tectonized events around Talimu Basin,and each tectonic movement controls the style of sedimentary basin and the changes of basin properties in Talimu craton. This paper discuss,es the stages of tectonic evolution from pre-Sinian to Car-bonifeous and the properties of primary basin during Carbonifeous.Furthermore,it shows that tec-tonic migration is an important character of the tectonic evolution of Talimu Basin.

塔里木盆地自前震旦—石炭纪经历了多期次的构造演化,前震旦纪盆地基底固结,震旦—奥陶纪为克拉通内坳陷、坳拉槽、被动大陆边缘;志留—泥盆纪为克拉通边缘隆升及石炭纪的克拉通内幼陷阶段。每次构造演化都与其周边的构造活动事件密切相关,从而控制了塔里木陆块内的沉积盆地样式及盆地属性的演化。本文讨论了塔里木盆地前震旦—石炭纪构造演化的阶段性,以及石炭纪原型盆地的属性,指出构造迁移现象是塔里木盆地构造演化的一个重要特征。

Palaeogeographically the South China palaeocontillent represents the extensive region of the southern parts of the Kunlun and Qinling Mountains,and is generally named South China. It includes the Yangtze, Cathaysian, Qiangtang-Qamdo landmasses as well as the Lhasa landmass separated from the Gondwana lalidmass group,and the Gyangze region onthe northern margin of the indian landmass. In the convergence of the China palaeocontinent,the Tarim and Qaidam landmasses were separated from the Yangtze landmass groupand...

Palaeogeographically the South China palaeocontillent represents the extensive region of the southern parts of the Kunlun and Qinling Mountains,and is generally named South China. It includes the Yangtze, Cathaysian, Qiangtang-Qamdo landmasses as well as the Lhasa landmass separated from the Gondwana lalidmass group,and the Gyangze region onthe northern margin of the indian landmass. In the convergence of the China palaeocontinent,the Tarim and Qaidam landmasses were separated from the Yangtze landmass groupand drifted to converge with the North China landmass at the end of the Early Palaeozoic.The subduction of the oceanic crust and the convergence of the landmasses have thefeatures of multistage development and the processes of collision and inlay in the form ofpoint,line and surface. The South China palaeocontinent underwent three stages of evolution. The first stage covers the late Late Proterozoic to Early Palaeozoic,when the PanYangtze landmass group was regulated for the first time. The isolated Tarim and Qaidamlandmasses were split from the western Yangtze landmass. Meanwhile,the eastern Yangtzelandmass was converged with the Cathaysian landmass to form the South China palaeolandmass,and further to come into collision with the extended North China landmass atone point. In the second stage during the Late Palaeozoic,the Pan-Yangtze landmass group was broken up, and the narrow Jinshajiang ceanic basin extended. The Qiangtang-Qamdoand Zongza laadmasses were separated from the Yangtze landmass. The third stage beginswith the Ladinian (Middle Triassic). Due to the subduction of the western Palaeo-PacificOcean, the migration of the South China landmass from east to west and the south-and northward subduction of the remnant Bayan Har oceanic basin,the epicontinental arc was formed along the Kunlun-West Qinling Mountains in the northern part,and the island-arc zone occurred along the Jinshajiang-Yushu region in the southern part. Then the Bayan Har sea basin was infilled and disappeared to transform into a foreland basin,resulting in the formation of the obductively orogenic zone on the western margin of the South Chinalandmass. However, the Lhasa landmass and Gyangze region were converged with theSouth China landmass during the late Late Mesozoic to Tertiary.

中国南大陆为—构造古地理名称,在地理上包括昆仑、秦岭山脉以南的广大地区,泛称中国南方。这些地区在地质历史演化中分属于扬子陆块、华夏陆块、羌塘—昌都陆块、中咱微陆块,也包括由冈瓦纳陆块群裂解出来的拉萨陆块和印度陆块北缘的江孜地区(雅江以南的中国境内)。塔里木陆块和柴达木陆块在中国古大陆的聚合中裂解、漂移,在早古生代末脱离扬子陆块的群体,与华北陆块聚合。因此,中国南大陆古地理的重建,不仅涉及南方各块体的聚合,还涉及中国古大陆的形成与劳亚大陆和冈瓦纳大陆会聚的关系,以及古特提斯洋的消亡。正是由于中国古大陆记录着多块体的聚合和叠置的洋壳消减带,因而表现出中国大陆上不仅克拉通盆地的稳定性低,也具边缘活动性高的特点。

 
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