泛古陸 的英文怎麼說

中文拼音 [fàngǔliù]
泛古陸 英文
pangaea
  • 泛 : Ⅰ動詞1 [書面語] （漂浮） float; drift 2 （透出; 冒出） be suffused with 3 （淹沒） inundate; floo...
  • 古 : Ⅰ名詞1 （古代） antiquity; ancientry 2 （先哲的遺典、道統） books or orthodoxies of ancient sages...
  • 陸 : 陸數詞（六的大寫） six （used for the numeral 六 on cheques, etc. to avoid mistakes or alterations）
  1. You will drive past the great divide watershed of the american continent to arrive at mammoth hot springs to view the multi - colored lava flow from extinct volcanoes, examine fossilized trees, and catch the glimmer of beautiful lakes in the secluded woods

    穿越美國大陸的分水嶺，到達公園最北的mammoth hot springs ，五顏六色的梯田，溫泉及滾燙的熔巖，石化的古木，碳化的火山口，林間的小湖，泛上裊裊的輕煙，宛如神話世界。
  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陸的主要部分都位於赤道附近及南半球，大致表現為沿緯度、呈東西向排列的特徵，中國及鄰區的小陸塊群在古生代始終都處在勞倫大陸、西伯利亞與岡瓦納大陸之間；隨著西伯利亞大陸的快速北移，在勞倫大陸與岡瓦納大陸的西部地區發生南北向拼合，亞皮特斯洋和里克洋的消亡，到古生代晚期形成統一的泛大陸；而岡瓦納大陸的東部（澳大利亞和印度等）則逐漸向南移動、離散，地殼張開，構成古特提斯洋；中國及鄰區的小陸塊群則一直處在古特提斯洋中，保持離散狀態，總體上緩慢地向北運移，並逐漸轉為近南北向的排列方式，石炭紀到三疊紀才在天山興安嶺、昆侖山、秦嶺大別、金沙江和紹興十萬大山等地段發生一系列局部性的陸陸碰撞，使中國大陸地塊的大部分逐漸併入歐亞大陸。
  3. Several important tectonic events took place in the chinese continent during the early paleozoic, such as the amalgamation of xiyu plate, forming a unified crystalline basement with the cathaysian plate, development of widespread intraplate deformations in southern yangtze plate, and the occurrence of altay - ergun collision zone

    它們與蘇格蘭阿帕拉契亞的加里東事件完全不同，在中國大陸出現了西域板塊完成拼合，華夏板塊構成統結晶基底，南揚子板塊廣泛發育板內褶皺，此時還形成了阿爾泰額爾古納碰撞帶等重要構造事件，而以中朝和北揚子板塊為代表的其他板塊則主要表現為穩定沉積，地塊運移，並呈離散狀態。
  4. In ancient times, lions used to be found all over asia, europe, and africa

    遠古時代，獅子曾廣泛分佈於亞、歐、非洲大陸。
  5. Terrestrial sediments can be found in shengli oil filed beginning from permian to tertiary. in addition, source beds are widely distributed

    勝利油區從古生代二迭紀到新生代第三紀每個地質時期都有陸相沉積，也廣泛地發育著生油層。
  6. The scholars insisting on transgression provided many markers such as mineralogy, lithology, paleoecology and geochemistry, but these makers are not completely the same as normal marine makers, moreover, the passageway and obviously increased makers of transgression have not been discovered, so " marine flooding ", " tsunami " and " terrestrial facies " appear, these viewpoints have coexisted for a long time

    盡管「海侵」論者提供了礦物學、巖石學、古生態學以及地球化學等多種標志，但是因為這些標志與標準海相標志比較，都有一定差別，而且至今沒有發現確實可靠的海侵通道和明顯的海相性遞增現象，所以又出現了「海泛」論、 「海嘯」論和「陸相」論。
  7. Many countries in both civil law system and common law system have accepted this system since it established

    自古代日耳曼法創建這一制度以來，被大陸法系和英美法系諸國和地區廣泛接受。
  8. These basalts are mainly formed in the course of mantle upwelling and widely continental extensionism through analyzing tectonic setting and pale - geographical setting

    通過對構造背景及古地理環境分析，峨眉山玄武巖主要形成於地幔上涌和廣泛的大陸伸展作用過程中。
  9. When the research content and meaning of the orogenic - sedimentology far more is expanding, and enlarging to the global paelogeography. the evolution history in rifting - assemble of southern china continental landmass is investigated with a relationship between sedimentary basin and orogenic belt, which reflects not only a synchronizing but also asynchronies in contrast, the southern china landmass with the global paelogeography. meanwhile it is promoted that the pan cathaysian is an important part of the global paelogeography

    把造山帶沉積學研究內容和內涵進一步擴展，放到全球的古地理格架中，從造山帶和沉積盆地關繫上研究中國南大陸的獨特裂聚演化史，反映出中國南大陸與全球古地理對比既有同步性也有非同步性；進而提出泛華夏陸塊群是全球古地理的一個重要組成部分。
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