1.The Yangtze landmass collided with North China landmass due to Caledoniansubduction which happened after the ocean basin closed with Paleotethys subduction atEarly Palaeozoic. At last it developed Caledonian orogeny and caused borderland basinreversing.
早古生代洋盆随原特提斯的消亡,经加里东期的俯冲,扬子地块与华北地块碰撞,最终形成加里东俯冲造山带,由此导致陆缘盆地的反转。
2.the upper time limit of the Erlangping retroarc basins in North Qinling is 320 Ma The three kinds of foreland basins of this type were formed under the background of landmass arc landmass collision in late Caledonian early Variscan, they formed the Qinling polygenic foreland basin system, the total course reaches 120 Ma
北秦岭二郎坪弧后前陆盆地的上限是 32 0 Ma,是在加里东晚期—华力西早期于陆—弧—陆碰撞的背景下形成 3种类型的前陆盆地 ,它们组成了秦岭复式前陆盆地 ,总历程达 1 2 0 Ma。
3.To push forward modernization in such a populous country with such a vast landmass, it is imperative to have strong core of leadership.
在人口如此众多版图如此辽阔的国家推行现代化必须要有坚强有力的领导。
4.Ironically, the eastern part of Russia is usually excluded from the definitions of the Orient and East Asia, even though Russia extends farther to the east than any other country on the Eurasian landmass.
可奇怪的是，俄罗斯的东部往往不算是东方和东亚，尽管俄罗斯比欧亚大陆块的任何一个国家向东延伸得都更远。
5.A small branch ocean basin in Menggubao-Pushouyuan,Tethyan ocean of northern Kangxiwa,western Kunlun mountain is firstly discovered in geological mapping of the Kangxiwa quadrangle at a scale of 1∶250,000,the east end of which connects to the early Paleozoic Kudi-Qimanyu ophiolite zone and the west end to the junction between Kangxiwa and Subashi. It divided the middle Kunlun micro-landmass into two secondary micro-landmasses in the east and west.
在1∶25万《康西瓦》幅区域地质调查中,首次在西昆仑康西瓦北侧昆中微陆块南部发现了一条蒙古包—普守原特提斯洋的一个分支小洋盆,其东端与早古生代库地—其曼于特蛇绿岩带相接,西端与康西瓦—苏巴什结合带相通,将中昆仑微陆块分割成了东西两个次级微陆块。
6.The small landmass depicted on the southernmost part of the map is considered to be an imaginary continent, which was assumed to counterbalance the continents of the northern hemisphere, since the time of ancient Greeks (Terra Australis).
从古希腊时期起，小陆地被描绘在地图的最南端，被认为是一块假想的大陆，假定是用作平衡南半球。
7.The Himalayan Mountains were formed some 150 million years ago after the landmass that is now India broke off from Antarctica, drifted north and collided with the rest of Asia.
喜马拉雅山脉大概在1亿五千万年前，当印度大陆从南极洲分离向北漂移时和亚洲其他部分撞击形成的。
8.Lawence Seaway tears further, essentially the weak link in this landmass held at so many points to the further side of the Atlantic.
从本质上来说，北美大陆是通过许多点和大西洋的另一端虚弱地连接着的。
9.Dahongshan Rock Group is the crystalline basement in the SW margin of the Yangzi Landmass.
大红山岩群是扬子陆块西南缘的结晶基底。
10.The Chuzhou Chaohu foreland fold thrust zone lies at the northeastern margin of the Yangtze Landmass and its basic tectonic framework is composed of thin-skinned structure of multilayered thrust decollement system that is controlled and formed by the deep, middle and shallow seated structural decollement zones at the top of upper Archean, upper Proterozoic and upper Palaeozoic groups in the area, respectively.
滁州——巢湖前陆褶皱冲断带位于扬子地块北东缘 ,受区域内上太古界、上元古界、上古生界顶部的深、中、浅三个构造层次滑脱带控制而形成的多层次逆冲 -滑脱系统组成的薄皮式构造 ,构成它的基本构造格架。
