collision zone 中文意思是什麼

collision zone 解釋
板塊碰撞帶
  • collision : n. 碰撞;沖突,抵觸,(政黨等的)傾軋。 come into collision with 和…相撞[沖突,抵觸]。 in collision with 和…相撞[沖突]。
  • zone : n 1 【地理】(地)帶。2 區域,范圍,界。3 〈古、詩〉(腰)帶。4 圈,環帶。5 【數學】(球面)帶;...
  1. Architecture, kinematics and deformation analysis in dabie - sulu collision zone

    運動學和巖石變形分析
  2. Study on collision tectonics in the east asia : tanlu - shangtaer collision zone

    尚塔爾碰撞帶研究
  3. 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。
  4. 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。
  5. During this evolution, seven second - order tectonic units were formed ; from north to south are the mingqianri cretaceous residual sea basin, the arsuo tectonic melange zone, the taricuo - wenbu yenshan magmatic arc belt, the cuoqin - bangduo late paleozoic composite back - arc basin, the jiangrang - geerdi faulted uplift, the gangdise - chazi himalayan magmatic arc belt, and the xigaze - anba fore - arc basin. these units comprise important parts of a poly - arc - basin system and exhibit evolutional features of mesozoic to cenozoic arc - basin systems. mosaic pattern of these tectonic units delineates the lithosphere coupling processes of the gangdise tectonic belt under mechanisms such as back - arc basin attenuation and arc - continent collision

    自中新生代以來,岡底斯構造帶經歷了洋殼俯沖、弧陸碰撞、陸內俯沖-碰撞、走滑和塊段隆升的多階段構造演化歷程,形成了由北向南七個二級構造單元,即岷千日白堊紀殘余海盆、阿索構造混雜巖帶、它日錯?文部燕山期巖漿弧帶、措勤?幫多晚古生代復合弧后盆地、江讓?格爾耿斷隆、岡底斯?查孜喜馬拉雅期巖漿弧帶、日喀則?安巴弧前盆地。
  6. The shear zone is a secondary structure zone of the syn - collision stage of southern tarim block with ili - isaik block

    該剪切帶屬南側塔里木與伊犁伊塞克兩陸塊碰撞縫合構造同碰撞期的次級構造帶。
  7. The zone would be a one - meter box that would collapse during a collision and absorb energy

    一個一米見方盒子大小的碰撞區將在碰撞發生時倒塌以吸收撞擊產生的沖力。
  8. Thus, the formation of the rock is related to lithospheric extension or collision events, which was derived from upper mantle and intruded along changle - nanao frature zone

    巖體是受俯沖流體交代的上地幔,經部分熔融沿長樂?南澳斷裂?應力轉換帶侵入。
  9. Indus - tsangpo suture zone is the joint of indian plate and eurasia plate. the study on its evolution history can provide us dynamic evidence for continent - continent collision between indian plate and eurasia plate. then what is the formation mechanism and deformation history for the indus - tsangpo suture zone

    雅魯藏布江結合帶是印度板塊和歐亞板塊碰撞的結合部位,研究其演化歷史能夠為解釋印度-歐亞板塊的陸-陸碰撞提供動力學方面依據,那麼本區雅魯藏布江結合帶的形成機制和變形歷史又是怎樣的呢
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