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Youtube.com的专用频道: Free Download — whitehouse — April 26, 2010 — Vice President Biden gives brief remarks and President Obama delivers the eulogy during a memorial service in Beckley, West Virginia for the 29 victims of the Upper Big Branch Mine explosion.

大陆的网友如果看下面视频是个空白,可以到二楼下载视频,一共约70M,可以反复看几遍,还是划算的。

Edg was set up in 1994 to serve the rapidly emerging building market of the new China.

康新设计工程有限公司自1994年进入中国大陆,结合了来自台湾、香港、美国、英国及大陆的建筑及设计专业人士,因应中国大陆经济改革及各式建筑的迅速发展,为这一新兴市场提供专业服务。

We are the first Continental European insurer to set up representative offices in Mainland China.

苏黎世在中国苏黎世在中国大陆的发展可以追溯到1993年,是第一家在中国大陆设立代表处的欧洲大陆保险公司。

It is now commonly believed that all continents of the earth were once combined into a single continent called Pangaea .

这是现在普遍认为,所有大陆的地球一度被合并成一个单一的大陆所谓的盘古大陆。

This thesis is focused on detailed studying recent tectonic deformation and earthquake activity of North China.

一、中国大陆的活动地块与强震活动在前人对中国大陆活动地块划分的基础上,研究了中国大陆活动地块与强震活动的关系。

Results show that the Spiti shale in Zanskar terminated 15Ma later than that in southern Tibet, while the lowermost Cretaceous quartz sandstone in Zanskar appeared 18Ma later than that in southern Tibet. The age of volcanic sandstone in southern Tibet is very poorly time constraint and their deposition occurred somewhere within Berriasian~early Albian. In Thakkhola, the Chukh Group volcanic sandstone are of late Hauterivian-early Albian age (duration about 20Ma), while in Zanskar, the volcanic sandstones facies only appeared in Albian (duration of less than 10Ma). Therefore, it can be concluded that the onsets of both quartz sandstone and volcanic sandstone occurred earlier in eastern Tethys Himalayas than in western Tethys Himalayas .

侏罗纪末~白垩纪初印度大陆的北缘同时期存在大陆向上挠曲,导致陆源碎屑输入量的快速增加,石英砂岩广泛存在;早白垩世火山岩屑砂岩对应着的印度大陆北缘地层侵蚀加深,使得较深部的深成火山岩暴露并遭受侵蚀;石英砂岩和早白垩世岩屑砂岩所代表的印度大陆剥露时间在空间上的&东早西晚&,说明构造运动首先是从特提斯喜马拉雅的东部开始(大印度与澳大利亚的彻底分离),然后逐渐波及西部的,东西时间差为15~20Ma;由于地壳均衡作用,大陆分离后原先地壳挠曲转变为地壳下沉,发生强烈的构造沉降,故Albian之后沉积一套深水环境下的海绿石、磷酸盐和黑色页岩沉积。

Based on the settings and geological and geochemical characteristics of granitoids of different orogenic belts (exemplified by orogenic granitoids in Altay, East Kunlun, Yanshan in North China, Northeast China and Nanling in South China), the relationships between granitoids and continental crustal growth are discussed, and five modes of continental crustal growth in the continent of China are proposed;they are as follows:(1)the Altay mode of continental growth is that the material and heat of the Paleozoic convertive mantle formed on the background of the Paleo-Asian Ocean were input into the Paleozoic continent and mixed with the materials of the upper crust;(2) the East Kunlun mode is that the basement of the Proterozoic orogenic belt was reworked by the heat input and materials of the Paleozoic-early Mesozoic convective mantle formed on the background of TTG continental crust of the Proterozoic orogenic belt;(3) the Northeast China style is that the Phanerozoic continental crust was reworked by the heat input and materials from the convective mantle formed on the background of the Yanshanian Central Asian orogenic belt;(4) the Yanshan mode is that the Archean basement was reworked by the heat input and materials from the Yanshanian convective mantle;and (5) the Nanling mode is that in South China what was input by the Yanshanian convective mantle into the continent was mainly heat and subordinately materials and the crustal material recycle was the dominant mode for the continental growth (showing zero continental growth).

根据不同造山带花岗岩的形成背景,地质地球化学特征差异,以阿尔泰,东昆仑,华北燕山,东北和南岭造山带花岗岩为例讨论花岗岩与大陆地壳生长的关系,区分出中国大陆的5种大陆地壳生长方式:阿尔泰式是古亚洲洋背景上形成的古生代对流地幔物质,热输入和上地壳混合为主的方式;东昆仑式是元古代造山带TTG陆壳背景基础上古生代—早中生代对流地幔物质和热输入,改造元古宙造山带基底的方式;东北式是燕山期中亚造山带背景上对流地幔物质和热输入改造显生宙陆壳的生长方式;燕山式是燕山期对流地幔物质和热输入改造太古宙基底的方式;南岭式燕山期对流地幔输入大陆的是以热为主,物质为辅,大陆地壳生长是以陆壳物质再循环为主的生长方式。

The main tectonic features of the four stages mentioned above can be summarized as follows, gneissic basement and greenstone belt in the Archean, formation and rifting of ancient continental crust in the Transition, creation and disposal of the first supercontinent Columbia in the Paleoproterozoic-Mesoproterozoic, and the assembly and disassembly of the supercontinent Rodinea under plate tectonic framework in Neoproterozoic.

这四大阶段的主要构造面貌分别是:片麻岩基底和绿岩带盆地,古陆壳的形成与裂解,第一个超级大陆即哥伦比亚超大陆的形成与离散,板块构造体制下罗迪尼亚超大陆的汇聚与离散,反映了大陆岩石圈的形成和由低级向高级的演化,因而每一阶段都有不同于前一阶段的沉积建造、火成岩类型及组合、变质作用、构造样式、构造线方向、变形方式和成矿作用。

Lin Zhengxian column group director told us that they this section is mainly introduced to audiences in Taiwan of Taiwanese business in China, development work and living conditions of the audience to introduce the mainlands scenic spots and cuisine.

台湾人在大陆》栏目组导演林政贤先生告诉记者,他们这个栏目主要是向台湾观众介绍台湾人在大陆创业、发展的工作和生活情况,并向观众介绍大陆的风景名胜和美食文化。

Meanwhile, the geothermal anomalies of fracture zone between massifs and intramassif reflect obviously. According to the temperatures under more than 40cm from the surface it can be divided into four parts.

印度次大陆自侏罗纪从非洲大陆裂离,至始新世与亚洲大陆接壤,导致了印度次大陆与亚洲主大陆的碰撞,而它持续、强烈的俯冲是青藏高原形成与隆升过程及现今各种状态的主导驱动力。

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在对危险的南部地区访问时,他斥责什叶派民兵领导人对中央集权的挑衅行为。

In fact,I've got him on the satellite mobile right now.

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