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the Continent相关的网络例句

查询词典 the Continent

与 the Continent 相关的网络例句 [注:此内容来源于网络,仅供参考]

The mid-19th century the European continent, the advent of the Great Revolution turmoil on the eve of Italy in the rule of the Austro-Hungarian Empire, the young Anzheluo plotting riots because the plan was brought to light and went into exile in France Aicheng, as childhood friend the betrayal, still can not escape were chased and killed by the Government of Austria sent destiny, in order to avoid killing, he inadvertently trapped in a plague-infested areas, the ravages of cholera that people fall into frenzy, Anzheluo been confusion is the misconception that the masses poisoning, has been the object of the chase strangling.

19世纪中叶的欧洲大陆,大革命风暴来临的前夕,意大利在奥匈帝国的统治下,年轻的安哲罗因为策谋暴动的计划败露而流亡到法国艾城,由于儿时朋友的出卖,依旧脱逃不了被奥地利政府派人追杀的命运,为了躲避追杀,他无意中陷入了一个瘟疫横行的地区,霍乱的肆虐使人们陷入狂乱,安哲罗被混乱的群众误认为是投毒者,成了被追捕绞杀的对象。

Diamonds began growth when "Jiangnan continent" combined to Yangtze craton, the growth and residence average temperature T〓 was about 1200℃; Diamonds were mutil-stages growth and interruption caused by temperature and pressure varied during Yangtze craton activities; Diamonds were etched when the magma did not erupt on the surface and form failed magma in mantle; during the later growth term T〓<1050℃, the type ⅠaA diamonds formed unclear and growth; Before the host magma erupted T〓<0.5Ma, T〓A<850℃, the type Ⅰb diamond formed unclear and growth; Few diamonds were brittle deformation during growth term, some were plastic deformation after growth; when the host magma erupted on the surface and weathered to alluvial deposit, diamonds surfaces formed green spots caused by irradiation, then most of green spots became to brown spots during a mid-temperature metamorphism; modern river reform it to alluvial deposit in the minute valley again.

在扬子地台&江南古陆&克拉通化时,金刚石开始生长,其生长与保存的平均温度T〓在1200℃左右;期间由于地台的活动,生长的温度压力条件发生了多次变化,使金刚石出现多次生长、停顿;夭折的母岩上侵活动使金刚石受到熔蚀作用;在金刚石形成的晚期,T〓值下降到1050℃以下,出现了另一次金刚石的生长期,在临近金刚石母岩上侵时T〓<0.5Ma,温度进一步降到850℃以下,使Ⅰb型金刚石得以保存;在金刚石形成期间还有过碎性变形发生;金刚石形成后部分样品经过了塑性变形;金刚石在上侵过程中,遭受了强烈的熔蚀;在母岩露出地表,形成沉积砂矿时,受到了放射性物质的辐照,先形成表层的绿色斑点、壳层,后经过中低温的热变质作用,大部分绿色转化为褐色;现代河流作用对沉积砂矿进一步改造,形成现在的细谷型砂矿。

In comparison with the observations derived from NOAA AVHRR, under the framework of NCAR CLM3, SCF schemes like CLM3 default, Douville1995, and Roesch 2001 underestimate SCF over vast areas, snow lines simulated in these three schemes are located to the south of that in the AVHRR observation, especially in autumn when snow pack begins to establish; Wu2004 scheme also underestimates SCF in the Eurasian continent in autumn; Yang1997 scheme slightly overestimates SCF, especially along the southern border of the snow covered area; Niu2007 scheme which accounts for the seasonal variation of snow density overcomes the positive bias of SCF simulated by Yang1997 scheme to some extent.

结果表明,在NCAR CLM3的物理过程框架之下,CLM3、Douville1995、Roesch2001三种方案低估了广大地区的积雪覆盖率,模拟的雪线位置偏北,尤其是在秋季积雪初期;Wu2004方案低估了秋季欧亚大陆的积雪覆盖率;Yang1997方案模拟的积雪覆盖率有些偏高,尤其是在积雪覆盖区的南部边缘;考虑积雪密度变化的Niu2007方案一定程度上克服了Yang1997方案的正偏差。

In the paper, Professor Zhao's historical course engaged in coral reef study and academic results are reviewed: he established the representative section for geological research on Quaternary coral reef, developed engineering geology research on coral reef, elaborated systematically landform development rules of coral reef in the South China Sea, uncovered certain paleo-oceanographical conditions and the new tectonic movement features, studied the historical climate recorded by lagoon of coral reef in the South China Sea and marine geography of coral reef for the first time, investigated comprehensively the only fringing reef of the seacoast of South China continent on western shore of Xuwen County, summarized initially the history of modern coral reef research in China.

文中回顾其从事珊瑚礁研究的历程,并评述其珊瑚礁研究的学术成果:建立了我国第四纪珊瑚礁地质研究的典型剖面;开拓了我国珊瑚礁工程地质研究;系统论述了南海珊瑚礁地貌发展规律,揭示了某些古海洋学状况和新构造运动性质;首次研究了南海珊瑚礁潟湖沉积记录的历史气候;首次进行了我国珊瑚礁区综合海洋地理学研究;较全面开展华南大陆沿岸唯一岸礁徐闻西岸珊瑚礁调查研究;初步总结了我国现代珊瑚礁研究史。

In the 17-18 century, they have developed into the European continent at the time of the country. In the early 19th century, when Napoleon occupied Germany, the abolition of the German title of Holy Roman Emperor, the name of the Holy Roman Empire had ceased to exist on. In the latter half of the 19th century, Prussian war through three dynasties, the realization of Prussia in Germany under the control of the uniform. Denmark to the war in 1864, Prussia and Austria to force Denmark ceded Schleswig - Holstein region.

在17-18世纪时,它们都发展成为当时欧洲大陆的强国。19世纪初,当拿破仑占领德意志时,取消了德意志的神圣罗马帝国皇帝称号,有名无实的神圣罗马帝国就不复存在了。19世纪后半期,普鲁士通过三次王朝战争,实现了德国在普鲁士控制下的统一。1864年对丹麦战争后,普鲁士和奥地利迫使丹麦割让石勒苏益格—荷尔斯泰因地区。

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The Last Lost Continent
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