皮亞代納 的英文怎麼說

中文拼音 [dài]
皮亞代納 英文
piadena
  • : Ⅰ名詞1 (人或物體表面的一層組織) skin 2 (皮革) leather; hide 3 (毛皮) fur 4 (包在外面的一層...
  • : Ⅰ動詞1 (代替) take the place of; be in place of 2 (代理) act on behalf of; acting Ⅱ名詞1 (歷...
  • : Ⅰ動詞1 (收進來; 放進來) receive; admit 2 (接受) accept; take in 3 (享受) enjoy; take deligh...
  1. And our wool that was sold in rome in the time of juvenal and our flax and our damask from the looms of antrim and our limerick lace, our tanneries and our white flint glass down there by ballybough and our huguenot poplin that we have since jacquard de lyon and our woven silk and our foxford tweeds and ivory raised point from the carmelite convent in new ross, nothing like it in the whole wide world

    還有尤維利斯371那個時在羅馬出售的咱們的羊毛,咱們的麻布和那在安特里姆的織布機織出來的花鍛,以及咱們的利默里克花邊372呢?咱們的鞣廠和遠處的巴利布373附近所生產的白色火石玻璃呢?
  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始終都處在勞倫大陸、西伯利與岡瓦大陸之間;隨著西伯利大陸的快速北移,在勞倫大陸與岡瓦大陸的西部地區發生南北向拼合,特斯洋和里克洋的消亡,到古生晚期形成統一的泛大陸;而岡瓦大陸的東部(澳大利和印度等)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大陸。
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