歐克瓦特 的英文怎麼說
中文拼音 [ōukèwǎtè]
歐克瓦特
英文
okvath- 歐 : 名詞1. （姓氏） a surname 2. （歐洲的簡稱） short for europe
- 克 : 克i 動詞1 （能） can; be able to 2 （克服; 克制） restrain; control 3 （攻下據點; 戰勝） overcome...
- 瓦 : 瓦動詞（蓋瓦） tile; put tiles on a roof; cover （a roof） with tiles
- 特 : Ⅰ形容詞（特殊; 超出一般） particular; special; exceptional; unusual Ⅱ副詞1 （特別） especially; v...
- 瓦特 : （功率單位） [電學] w （watt）瓦特計 wattmeter
-
From lianyungang, transshipped via shanghia, the cargo to europe ports such as felixstowe, antwerp, rotterdam, hamburg ; australia ports such as sydney, melbourne ; middle east ports such as dubai, bandar abbas, kuwait, bahrain, karachi, damman, doha, nhavasheva ; east america ports such as new york, savannah, norfolk ( transhipment to inland points of eastern american ) ; southeast asia ports, such as port - kelang, penang, surabaya, jakarta, bangkok, leamchabang, chittagonhg, colombo could be shipped
由連雲港到上海中轉可以接轉費力克斯托、安特衛普、鹿特丹、漢堡等歐洲港口；悉尼、墨爾本、布里斯班等澳州港口；迪拜、阿巴斯、科威特、巴林、卡拉奇、達曼、多哈、孟買等中東港口；紐約、薩瓦那、諾福克（轉接其他美東內陸點）等美東港口；巴生、濱城、泗水、雅加達、曼谷、林查班、吉大、科倫坡等東南亞港口。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。
分享友人