泛大陆的英文

• pangaea

• "泛"英文翻译    float; drift
• "大陆"英文翻译    continent; mainland
• "泛大陆解体" 英文翻译 :    pangea break-up
• "泛大洋" 英文翻译 :    panthalassa
• "大陆" 英文翻译 :    1.(广大的陆地) continent; mainland2.(姓氏) a surname 大陆永久 dalu yongjiu
• "广泛大众题材" 英文翻译 :    common human themes
• "大陆性；大陆度" 英文翻译 :    continentality
• "超大陆" 英文翻译 :    super continent; supercontinent
• "次大陆" 英文翻译 :    [地理学] subcontinent
• "大陆；大洲" 英文翻译 :    continent
• "大陆；继续" 英文翻译 :    cont． continent；continued
• "大陆报" 英文翻译 :    continent le; continental el; continentale; el continental; le continent
• "大陆冰" 英文翻译 :    continental ice; land floe
• "大陆岛" 英文翻译 :    continental island; continentalisland
• "大陆的" 英文翻译 :    continental
• "大陆堤" 英文翻译 :    continental embankment
• "大陆度" 英文翻译 :    continentality
• "大陆盾" 英文翻译 :    continental shield
• "大陆筏" 英文翻译 :    continental raft
• "大陆法" 英文翻译 :    civil law; continental law; continental method
• "大陆风" 英文翻译 :    continental wind
• "大陆海" 英文翻译 :    continental sea; epeiricsea; inland sea
• "大陆核" 英文翻译 :    continental nucleus; continentalnucleus; nucleus of continent
• "大陆河" 英文翻译 :    continental river; continentalriver
• "大陆湖" 英文翻译 :    continental lakes

• Thus , it can be clearly recognized that the global continents located at near equator and southern hemisphere , showed the characteristics of range along latitude ; chinese continental blocks still located among the laurentia , siberia and gondwana in paleozoic ; following the fast moving of siberia plate to northwards , the amalgamation in north - south direction at the western parts of laurentia and gondwana , subducted the lapetus and rheic oceans , until to form the uniform pangea in the late stage of paleozoic ; however australia and india plates in eastern gondwana move and disperse gradually to southwards , to extend crust and form the paleo - tethys ocean ; the chinese continental blocks and adjacent blocks still located in paleo - tethys ocean , preserved the status of dispersion , gradually moving to northwards , showed the characteristics of range along north - south orientation , until carboniferous and triassic a series of local collisions happened in tianshan - hing ' anling , kunlun , qinling - dabie , jingshajiang and shaoxing - shiwandashan zones , thus the most part of chinese continental blocks amalgamated to eurasia continent
  由此可以清晰地看出，在古生代早期全球各大陆的主要部分都位于赤道附近及南半球，大致表现为沿纬度、呈东西向排列的特征，中国及邻区的小陆块群在古生代始终都处在劳伦大陆、西伯利亚与冈瓦纳大陆之间；随着西伯利亚大陆的快速北移，在劳伦大陆与冈瓦纳大陆的西部地区发生南北向拼合，亚皮特斯洋和里克洋的消亡，到古生代晚期形成统一的泛大陆；而冈瓦纳大陆的东部（澳大利亚和印度等）则逐渐向南移动、离散，地壳张开，构成古特提斯洋；中国及邻区的小陆块群则一直处在古特提斯洋中，保持离散状态，总体上缓慢地向北运移，并逐渐转为近南北向的排列方式，石炭纪到三叠纪才在天山兴安岭、昆仑山、秦岭大别、金沙江和绍兴十万大山等地段发生一系列局部性的陆陆碰撞，使中国大陆地块的大部分逐渐并入欧亚大陆。

• 泛大陆的泰文
• 泛大陆的法语：pangée
• 泛大陆的日语：パンゲア
• 泛大陆的韩语：판게아 대륙
• 泛大陆的俄语：пангея
• 泛大陆的阿拉伯语：بانجيا;