歐亞大陸板塊 的英文怎麼說

中文拼音 [ōuyǎdàliùbǎnkuāi]
歐亞大陸板塊 英文
eurasian plate
  • 歐 : 名詞1. （姓氏） a surname 2. （歐洲的簡稱） short for europe
  • 陸 : 陸數詞（六的大寫） six （used for the numeral 六 on cheques, etc. to avoid mistakes or alterations）
  • 板 : Ⅰ名詞1 （片狀硬物體） board; plank; plate 2 （專指店鋪的門板） shutter 3 [音樂] （打拍子的樂器） ...
  • 塊 : 名詞（古時佩帶的玉器） penannular jade ring （worn as an ornament in ancient china）
  • 歐亞大陸 : eurasia
  • 歐亞 : eurasian歐亞大陸 eurasia
  • 板塊 : [地] plate板塊邊緣 plate margin; 板塊構造 plate tectonics; raft tectonics; 板塊假說 plate hypothe...
  1. The result of geodetic inversion shows that india block moves at rates of 20. 4 millimeters per year with respect to the stable eurasia, consistent with the result comes from geology. this indicates that the rate india block moves towards eurasia is stable

    這與從地質推斷的過去2 3百萬年期間內，印度板塊向歐亞大陸俯沖平均為18mm / y的速率大致相同，表明在較長時間范圍內，印度板塊向歐亞大陸俯沖的速率是穩定的。
  2. The collision between continental plates is a key to understanding the evolution of continental dynamics. perhaps the most spectacular large - scale result of plate tectonics is the broad complicated zone of intracontinental convergence between eurasia and peninsular india following their collision at about 45 ma

    大陸內部的陸-陸碰撞過程是大陸動力學的核心問題，青藏高原被視為印度板塊與歐亞板塊于新生代碰撞的結果，是典型的陸-陸碰撞帶。
  3. The continents of europe and asia are actually one large land mass

    歐亞大陸其實是一龐大的陸地板塊。
  4. Japan lies between eurasia plate and the pacific plate. it is mostly rugged and mountainous

    日本位於歐亞大陸板塊和太平洋板塊之間，大部分地區都是崎嶇不平的山地。
  5. Geologists and geophysicists have carried out substantial work on petrology, geochemistry, chronology and geophysics, et al., which yields important reference material and constrains for explanations of questions, such as the delamination and exhumation mechanism for the lower crust, models of the rapid uplift of himalayan orogen and deep subduction of india - eurasia plate. while only a little has been done to study the eastern syntaxis at present

    地質學家和地球物理學家已經對西構造結進行了大量的巖石學、地球化學、年代學和地球物理學等方面的研究，為解釋下地殼的拆沉、折返機制，喜馬拉雅造山帶的快速隆升和印度-歐亞板塊的大陸深俯沖模式等提供了重要的參考信息和約束條件。
  6. ( 4 ) the collision zones of eurasia are very complicated due to the extrusion of continent lithospheres and the subduction between the oceanand continent lithospheres, and we analyze the mutual effects of different lithospheres and the crustal deformation features of collision zones ( 5 ) firstly we give the present - day spreading velocity of the mid - atlantic ridge

    （ 4 ）系統分析了歐亞碰撞帶大陸與大陸和大洋與大陸兩種截然不同的巖石圈擠壓與俯沖對歐亞板塊的影響及其邊界地殼形變特徵。
  7. The west of sichuan is situated between the india board and asia - europe board, which link the sichuan basin and qingzhang plateau. so its geological structure and landscape is unique. there are plenty of ecological environment resources, nature landscape resources and culture resources

    川西地區處于印度板塊和亞歐大陸板塊之間，為四川盆地與青藏高原接合部位，其獨特的地質構造，造就了川西地區奇特的地質景現，蘊含著豐富的生態環境資源和景觀資源，為開展森林遊憩提供了可靠的物質基礎。
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