indian plate meaning in Chinese
印度板块
Examples
- I took all those old indian plates and bowls
我把那些印第安古董 - Areas beneath the mountain belts are under compression while areas beneath basins and the foredeep of the indian plate are under compression
区内造山带下方均处于挤压；盆地和印度板块前缘处于拉张。 - 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。 - 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
雅鲁藏布江结合带是印度板块和欧亚板块碰撞的结合部位，研究其演化历史能够为解释印度-欧亚板块的陆-陆碰撞提供动力学方面依据，那么本区雅鲁藏布江结合带的形成机制和变形历史又是怎样的呢 - The meso - cenozoic evolution of bachu fault - uplift is closely related to its south and north subsiding foredeep . under the background of indian plate subducting under asia - europe plate , bachu forebulge was greatly affected by the development of southwest depression and awati depression . almost all of its structure reversed , and as a result of it , both of its south and north boundary migrated . according to its evolution history and its feature , the authors tentatively use both - side migration model to interpret the evolution of compound forebulge . since triassic , almost all the spheres above lithosphere synchronously became flexure . because transpressional stress field became increasingly strong , bachu forebulge continued uplifting and big faults formed . then , bachu uplift , as a whole , slipped upward along those big faults and showed migrating toward thrust zone in plane . in tectonic tranquility , the lithosphere bounded back and in consequence of it , bachu uplift slipped down and showed migration toward craton , at that moment negative inversion structures developed . while the forebulge migrated toward its south and north foredeep , it was very possible that locally extensional stress appeared in the forebulge
在印度板块向欧亚板块俯冲的大背景下，巴楚前缘断隆受西南坳陷和阿瓦提凹陷的影响，新生代时构造体制发生反转，边界向南北迁移。根据其发育过程特征，作者用复合前缘隆起两端迁移模式对复合前缘隆起独特的构造发育史进行了解释：即三叠纪以来岩石圈各圈层同步挠曲变形。随着挤压应力场的增大，巴楚隆起在挠曲基础上不断抬升，形成几条大型断裂带。