印度洋板块 meaning in Chinese
indian ocean plate
Examples
- In the late early cretaceous , the ncc turned into contraction stage again by the influence of the subduction of pacific plate and indian plate
早白垩世晚期该区受太平洋板块和印度洋板块俯冲作用影响，华北板块再次转入挤压作用阶段，开始了滨太平洋域的演化。 - To benzilan ( where visitors can view the geological legacy of the collision of the european - asian plate with the indian sea plate ) , then on to the dongzhu temple group , and then proceeding to baimang snow - capped mountain , and the feilai temple in deqin , and on to meili snow - capped mountain , mingyongqia glacier , and xidang hot springs from which one can continue on to the yuben fairy waterfall
由中甸为起点，松赞林寺、纳帕海、奔子栏（游览欧亚板块与印度洋板块碰撞地质遗址） 、东竹林寺、白茫雪山、德钦飞来寺、梅里雪山、明永恰冰川、西当温泉、雨崩神瀑。 - By means of gps velocity field data , the synthetically crustal media parameters of the plateau were reversibly analyzed , as well as the simplified boundary function forces . thus , the moving tectonic characteristics of the plateau were analyzed macroscopically . finally , the main conclusions are that the majority of tectonic deformation of the plateau is the n - s compression and the minority is the w - e stretching
首先通过gps速度场反分析了高原地壳的综合介质参数，并反分析了简化后的高原地壳的边界作用力，从宏观上分析了青藏高原的构造运动特征，分析结论认为：青藏高原的构造变形以南北挤压为主，东西扩张为辅；造成高原现今构造格局的主要原因是印度洋板块和欧亚板块的持续碰撞。