| 1. | 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。 |
| 2. | The 9 . 0 magnitude quake that caused the 2004 indian ocean tsunami occurred on the sea floor , where the india plate rubs against the burma plate
2004年导致印度洋大海啸的9级大地震发生在海底，这是印度板块和缅甸板块摩擦所造成的结果。 |
| 3. | It was thought that madagascar and india broke away from around 120 million years ago , while madagascar went its own way around 88 million years ago
据称，马达加1 . 2亿年前与其它大陆板块分离，到了8800万年前，马达加斯加又与印度板块分离。 |
| 4. | It was thought that madagascar and india broke away from the other continents around 120 million years ago , while madagascar went its own way around 88 million years ago
据称，马达加斯加和印度板块在约1 . 2亿年前与其它大陆板块分离，到了8800万年前，马达加斯加又与印度板块分离。 |
| 5. | The two island groups are the peaks of an undersea mountain range , raised by the scraping up of soft sediments as the plate ' s leading edge pressed down and forward against the india plate
这两个群岛是海底山脉的山峰，它们是缅甸板块挤压印度板块时，缅甸板块前端下沉至印度板块下方，并持续向前推进，其前沿的软质沉积物被刮起、逐渐累积而成。 |
| 6. | 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
这与从地质推断的过去2 3百万年期间内，印度板块向欧亚大陆俯冲平均为18mm / y的速率大致相同，表明在较长时间范围内，印度板块向欧亚大陆俯冲的速率是稳定的。 |
| 7. | 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。 |
| 8. | This “ sliver ” plate , a long , thin section of crust that reaches southward from myanmar ( burma ) , pushes over and against the india plate to its west at the rate of 14 millimeters a year ; on december 26 , 2004 , the burma plate jerked westward and upward along an incline by perhaps 15 meters
缅甸板块是形状长而细瘦的小板块，由缅甸往南延伸，以每年14公?的速度往西推挤印度板块； 2004年12月26日，缅甸板块猛然向西挤压，使其沿著断裂面向上位移了约15公尺。 |
| 9. | We deduce that it is a relic old crust that was brought upwards during the formation of neo - tethyan ophiolite . the step heating 40ar - ' 9ar spectra show that during 100ma , luobusha ophiolite suffered intensely alternation , which affected distinctly the k - ar system ; during 771ma some basalt formed in the country rock of xiubugabu ophiolite ; during 55ma , the pillow basalt of rikangba ophiolite affected by a strong thermal event ; all the variety of ages illustrates possible impacts of the subduction - collision between india and eurasia . through dissecting mainly the gabbro of luobusa ophiolite and studying the 40ar / 39ar
~ ( 40 ) ar ~ ( 39 ) ar阶段升温年龄图谱显示， 100ma左右罗布莎岩体经历了较强的后期蚀变作用，对其k ? ar体系造成明显影响； 77 1ma休古嘎布岩体围岩中形成玄武质火山集块岩； 55ma日康巴岩体岩石枕状玄武岩受到较强热事件影响；这些~ ( 40 ) ar - ~ ( 39 ) ar年龄上的变化显示了印度板块与欧亚板块俯冲?碰撞对该区的强烈影响。 |
| 10. | 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
川西地区处于印度板块和亚欧大陆板块之间，为四川盆地与青藏高原接合部位，其独特的地质构造，造就了川西地区奇特的地质景现，蕴含着丰富的生态环境资源和景观资源，为开展森林游憩提供了可靠的物质基础。 |
