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碰撞带的英文

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"碰撞带"怎么读用"碰撞带"造句

英文翻译手机手机版

  • collision belt
  • collision zone
  • collisionzone

例句与用法

  • Study on collision tectonics in the east asia : tanlu - shangtaer collision zone
    尚塔尔碰撞带研究
  • The high - pressured granulites are formed both in the convergent area such as the subduction zones and collision zones and in the spreading area such as the bottom of the island arcs
    高压麻粒岩既可形成于汇聚型构造环境如俯冲带、碰撞带等,也可形成于伸展型构造环境如岛弧底部。
  • 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
    大陆内部的陆-陆碰撞过程是大陆动力学的核心问题,青藏高原被视为印度板块与欧亚板块于新生代碰撞的结果,是典型的陆-陆碰撞带
  • 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
    它们与苏格兰阿帕拉契亚的加里东事件完全不同,在中国大陆出现了西域板块完成拼合,华夏板块构成统结晶基底,南扬子板块广泛发育板内褶皱,此时还形成了阿尔泰额尔古纳碰撞带等重要构造事件,而以中朝和北扬子板块为代表的其他板块则主要表现为稳定沉积,地块运移,并呈离散状态。
  • ( 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 )系统分析了欧亚碰撞带大陆与大陆和大洋与大陆两种截然不同的岩石圈挤压与俯冲对欧亚板块的影响及其边界地壳形变特征。
  • In this case during paleozoic , nearly east west trending arc structures resulted from the interaction between china plate and siberian plate . in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault , diaoyudao fault , okinawa fault , uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate
    本文所涉及近东西向展布的弧形构造形成于古生代时期中国板块与西伯利亚板块的碰撞带,而在中生代,中国板块下的kula - pacific板块向西俯冲导致了北北东向和北东向构造(如duimadao断层、 diaoyudao断层、 okinawa断层、隆起带和沉降带)以及位于中国板块东部的火山岩浆带。
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