1.After undergoing the tectonic motions and butt jointing of south north continent in Tethys stages, the collision between continent and continent in Upper Cretaceous period and Eocene epoch, the formation of plateau rudiment in Oligocene epoch and Miocene epoch, and the intra continental deformation of rapid uplifting since Pliocene epoch, the geomorphic landscape of "high massive flattish" Qinghai Tibet Area is formed.
并且青藏地区在经历了特提斯阶段的几次构造运动及南北大陆对接以后的白垩纪末 -始新世陆 -陆碰撞、渐新世 -中新世高原雏形的形成和上新世以来高原快速隆升的陆内变形作用以后 ,就形成了今天这种“高、大、平”的独特地貌景观。
2.Since the Great Britain is an island country out of the Continent, the content of its foreign strategy must come from this location: expanded actively to the oversea, managed its domain and strength, and at the same time, to the countries in the Continent, it adopted the balance of the powers, preventing the emergence of the super- hegemonical countries which would threaten the security and hegemony of the Great Britain.
由于英国是处于欧洲大陆之外的岛国,这一地理位置决定了它的外交大战略的内容:积极向海洋扩张,经营自己的版图和实力,同时对欧洲大陆采取均势政策,防止超霸型国家出现,威胁英伦三岛的安全和英国的优势地位;
3.Continent to continent collisions along subduction zones makes continents larger, while rifts along spreading centers break them apart again.
大陆与大陆沿俯冲带的碰撞使大陆扩大，而沿扩张中心的断陷使它们再次分开。
4.The U-Pb isotopic measurements of zircons from the same eclogite gave a concordia age of 503. 9 ± 5. 3 Ma. Two methods yielded a similar age, which reveals the peak metamorphic age of eclogites and reflects the existence of erogenic root related to continental subduction and continent-continent collision during the early Palaeozoic.
其变质锆石的U-Pb年龄为503.9±5.3Ma,两者基本一致的年龄数据反映了榴辉岩的峰期变质时代,从而表明了阿尔金西段加里东期与深俯冲和陆-陆碰撞作用有关的山根的存在。
5.Improving upon hull below and rigging above, he makes a proud merchantman, to be wafted by the winds from continent to continent.
通过改进船体水下部分，并在船体上安装上风帆，他就成了令人骄傲的商人，让风将他从一个大陆送往另一个大陆。
6.Started from Dec.28 1935 M_S7.7 Sumatra earthquake in the southern boundary of India-Australia plate and Eurasia plate, the migration got into the continent of China after arriving at Burma arc and eastern end of Himalayan arc towards north through Andaman trench. Then it reached directly Mongolia along the seismic belt of the mean axis of China-Mongolia continent.
迁移以1935年12月28日苏门答腊MS7.7地震为起点,从印度—澳大利亚板块与欧亚板块南部边界俯冲事件开始,向北经安达曼海沟到达缅甸弧和喜马拉雅弧东端后,进入中国大陆,沿着中蒙大陆中轴地震带直抵蒙古。
7.Tongling area, one of the 7 ore concentration areas in the Middle_Lower Yangtze metallogenic belt of eastern China, has tectonically undergone a geological history from Late Paleozoic continental rifting through Middle Triassic continent_continent collision to Jurassic_Cretaceous intra_continental tectono_magmatic activation.
铜陵矿集区是长江中下游成矿带七大矿集区之一 ,构造上经历了晚古生代的陆缘裂陷、中三叠世的陆_陆碰撞和侏罗纪—白垩纪的陆内构造_岩浆活动。
8.Viewing from the global scope, particularly looking at the situation in China, the granitic tectono-magmatic assemblages could be divided into five major types: (1) oceanic crust subduction type, such as continental margins on both sides of the Pacific Ocean; (2) continent continent collision type, e.g., the Himalaya-Gangdise collisional belt; (3) extensional continental margin type, such as the Southeast China extensional margin and the Basin and Range Province, USA; (4) inland faulted depression type, such as the Lower Yangtze faulted depression and the Qiantan-Xinjiang faulted depression; (5) rift type, such as the Eastern African Rift and the Panxi Rift of China.
从全球范围来看，结合中国的地质实际，花岗岩的构造岩浆组合可以区分为5种主要类型：(1)洋壳俯冲消减型，如太平洋两岸的大陆边缘；(2)陆－陆碰撞型，如喜马拉雅－冈底斯碰撞造山带；(3)陆缘伸展型，如中国东南部伸展型大陆边缘、北美西部盆岭省；(4)陆内断裂拗陷型，如长江中下游断裂拗陷、钱塘江一信江断裂拗陷；(5)裂谷型，如东非裂谷、攀西裂谷。
9.During Silurian Devonian,"Kunlun Ocean" was all consumed,and in the same time ,the western Kunlun Early Paleozoic magmatic arc collidedwith Tarim continent,then generated foreland thrust belt,Devonian foreland asin and Tarim continent Devonian"red bed" phase.
志留纪－早泥盆世，“昆仑洋”消失，西昆仑早古生代火山弧与塔里木大陆碰撞，并形成塔里木前陆冲断带和泥盆纪前陆盆地磨拉石及塔里木大陆内泥盆纪的“红层相”
10.By the continental dispersion, the spreading of ocean, the drift and the collision of the continental plates, the oceanic subduction and destruction, crustal uplift, orogenesis, the continental-continent collision and the depession in continent, the complited tectonic sedimentary environment and the plate tectonic units were formed in the processing of long geological historic evolution.
在漫长的地史演化过程中,大陆裂解和大洋扩张,大陆板块的飘移与碰撞,洋壳俯冲与大洋消亡,地壳隆升与造山,陆陆碰撞及陆内裂陷等活动频频发生,形成了极其复杂的构造沉积环境及板块构造体系。
