Chinese translation for "tethys ocean"
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- 古地中海
特提斯洋
Related Translations:
tethys: 古地中海特提斯海泰西丝土卫三 古地中海忒堤斯
- Example Sentences:
| 1. | The authors put forward that daba - xiugugabu ophiolite belt originated from an ancient oceanic crust fragment of india continental northern marginal ocean basin , that was approximately synchronous with the formation and evolution period of the neo - tethys ocean
笔者提出该区蛇绿岩来源于印度大陆北缘洋盆的洋壳碎片，这个陆缘洋盆与新特提斯洋主体的形成和演化准同步。 | | 2. | 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。 | | 3. | The marginal ocean basin ' s formation and evolution model may be as follows : early triassic , rift was formed by extension and splitting in india ( gondwana ) continental margin during it was drifting southward ; late triassic , the rift had been joined in the neo - tethys ocean in the east and converted into initial ocean basin , and ayila - zhongba micro - continental was formed in north of the rift
洋盆的演化模式是：早三叠世，随着印度（冈瓦纳）大陆向南漂移，其北部边缘因引张裂解产生裂谷，于晚三叠世向东开口与新特提斯洋主体连通，洋盆初具洋壳性质，北侧形成阿依拉仲巴微陆块。 |
- Similar Words：
- "tethis" Chinese translation, "tethong" Chinese translation, "tethyan" Chinese translation, "tethys" Chinese translation, "tethys (mythology)" Chinese translation, "tethys sea" Chinese translation, "teti" Chinese translation, "tetiana perebiynis" Chinese translation, "tetiaroa" Chinese translation, "tetiaroa atoll" Chinese translation
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