十万大山的英文

• shiwan dashan

• "十万"英文翻译    one hundred thousand
• "大"英文翻译    big; large
• "九万大山" 英文翻译 :    jiuwan dashan
• "六万大山" 英文翻译 :    liuwan dashan
• "万大" 英文翻译 :    wanta
• "年六月拿破仑发动六十万大军" 英文翻译 :    grande armée
• "十万" 英文翻译 :    one hundred thousand
• "大山" 英文翻译 :    barrow; da shan; dagi; dai son; daisen; dashanpusaurus; gora; lantau island; mark rowswell; massif; mountain; oyama; sunset peak; zan
• "奉万大" 英文翻译 :    man-dae bong
• "第十万" 英文翻译 :    one hundred thousandth
• "二十万" 英文翻译 :    200 thousand
• "几十万" 英文翻译 :    hundreds of thousands of
• "十十万" 英文翻译 :    shijima; tooma
• "十万万" 英文翻译 :    milliard
• "四十万" 英文翻译 :    aiman; shijima; shijuman; shishiya; yosuma
• "王十万" 英文翻译 :    wangshiwan
• "百万大饭店" 英文翻译 :    the million dollar hotel
• "百万大富翁" 英文翻译 :    who wants to be a millionaire - 2nd edition
• "百万大军" 英文翻译 :    army a million strong
• "百万大赢家" 英文翻译 :    who wants to be a millionaire
• "赫勒万大学" 英文翻译 :    helwan university
• "大山 (演)" 英文翻译 :    dashan
• "大山倍" 英文翻译 :    masutatsu oyama
• "大山部" 英文翻译 :    oyamabe
• "大山洞" 英文翻译 :    cavern

• From shanxi and gansu provinces , and 1 new species , hydromanicus angulatus yang l . & yang w . n sp
  记述广西十万大山1新种：角突离脉纹石蛾hy加manicusangulatusyangl
• The results indicate : ( 1 ) the distribution of magmatic rocks shows the feature that in the middle and western part of the study area basic igneous rocks dominate , and in the middle - eastern part intermediate rocks are predominant , while in the southeastern part acid ones are developed . ( 2 ) in the area west to the shiwandashan basin , intermediate magmatites were controlled by deep ne - striking and nw - striking faults , especially at the conjunction site of these two group faults , magmatic activity was strong ; and its tectonic background can be attributed to extensional continental rift
  其中，在十万大山盆地以西地区的偏基性岩浆活动受北东和北西向深断裂控制明显，尤其以此两组断裂交汇处的岩浆活动强烈，盆地构造背景属大陆伸展裂谷环境；在十万大山盆地以东地区为偏酸性岩浆活动，主要受东吴运动形成的钦防造山带的控制，属大陆边缘造山带或岛弧造山带环境。
• 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。