plate amalgamation 中文意思是什麼
plate amalgamation
解釋
板上混汞法- plate : n 1 厚金屬板 〈cf sheet〉 板（片）；（記有姓名等的金屬）牌子，（尤指醫生的）招牌，藏書牌；【印刷...
- amalgamation : n. 1. 【冶金】汞合，汞齊化。2. 混，合併。3. 〈美國〉（種族等的）融合 -tiveadj.
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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。 -
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。
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