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Exhibiting angle unconformities or erosion unconformities in different part of the basin, these surfaces are obvious to be recognized on seismic profiles.T1 conformity, separating Eogene from Neogene, was formed during the whole basin uplifting and erosion by the end of Eogene.T1 unconformity denuded unbearing strata differently, and the deeper and thickest erosion lies on the southern margin of the basin, which reflects the activity of southern Jiangnan paleo-terrene. In conclusion, the major erosion belts extending along NW direction reflects NE-SW compression and slipping caused the Eogene basin uplift and strengthen the earlier NW direction extending low convex, and formed the NW direction extending depress and erosion belts.

古近系和新近系之间的T1不整合面形成于古近纪末期的盆地整体抬升,对下伏地层造成不同程度的剥蚀,沿盆地南缘的剥蚀层位深,剥蚀量大,反映盆地南缘整体相对隆起,与江南古陆的隆起作用有关。T1界面剥蚀带走向以北西向为主,反映了盆地在古近纪末受到了北东-南西向的挤压或压扭作用,该作用造成盆地整体抬升,强化了北西向展布的低凸起,产生了近北西向的洼和剥蚀带。

The rift areas in the region, which are underlain by significantly thinned lithosphere, appear to be related to ancient mechanically weak zones.

这些古老岩石圈薄弱带可能经历了后期构造事件的多次改造,并在新生代印度-欧亚陆陆碰撞过程中被进一步弱化、减薄,最终造成地表裂

As soon as I stuck in the swamp of unfortunateness, what I did was to indulge myself and throwing my ambitions away.

当我在沼泽unfortunateness ,我就是这样做是为了放纵自己,我的野心扔了。

Accidentally, I read the poems of Xi murong in the world of utter desolation, whose unostentatiousness and deep feelings made me suddenly plunge into poetry River, and got in deeper and deeper.

茫茫荒原里无意中读到席慕容的诗,那种无华与深情让我一下子坠入诗歌之河,且越越深。

It is considered that the Tertiary unconformity in Jiyang Depression can be divided into three types: typeⅠ1, typeⅠ2 and typeⅡ. Unconformity generally consists of weathered clay, semi-weathered rock and unweathered rock.

研究认为济阳坳第三系不整合可划分为三类:Ⅰ1型结构、Ⅰ2型结构和Ⅱ型结构,完整的不整合结构包括风化粘土层、半风化岩石、未风化岩石。

At Point éphémère (200, quai de Valmy; 33-1-40-34-02-48; www.pointephemere.org ), a ramshackle bar-resto-concert-hall-art-space next to a fire station, I ate an excellent steak tartare and a maliciously rich chocolate tart and drank plenty of wine for a very reasonable 20 euros, then had 3-euro beers at Chez Prune (71, quai de Valmy; 33-1-42-41-30-47), right next to a bridge made famous by Marcel Carné's 1938 movie "HOtel du Nord."

在消防站附近摇晃的艺术、酒吧、音乐会合一的广场,我吃了美味的牛排和大大的巧克力饼,喝了很多葡萄酒,才花了20欧元。然后,就在靠近以电影HOtel du Nord而闻名的一座桥边的酒吧里,喝了3欧元的啤酒。

After some time, I came thither dress'd in my new Habit, and now I was call'd Governour again; being all met, and the Captain with me, I caused the Men to be brought before me, and I told them, I had had a full Account of their villanous Behaviour to the Captain, and how they had run away with the Ship, and were preparing to commit farther Robberies, but that Providence had ensnar'd them in their own Ways, and that they were fallen into the Pit which they had digged for others.

但上帝却使他们自投罗网,跌进了他们替别人挖掘的井。我让他们知道,在我的指挥下,大船已经夺回来了,现在正停泊在海口里。他们过一会就可以看到,他们的新船长被吊在桅杆顶上示众,他的罪恶行径得到了报应。至于他们,我倒想知道他们还有什么话可说。事实上,我完全可以把他们以海盗论处。当然,他们大概绝不会怀疑,我完全有权把他们处死。

Vulcanic lake, the dead sea : no fish, weedless, sunk deep in the earth.

火山湖,死海。没有鱼,也不见杂草,深深地进地里。

Vulcanic lake , the dead sea : no fish , weedless , sunk deep in the earth

没有鱼,也不见杂草,深深地进地里。

The research method and principle for vadose field of confined deep water are also discussed, and the waterhead contour and hydrodynamic zoning maps are outlined for the study interval, by which flow regimes and rules of deep water are revealed in the depression.

在阐述区域地质构造和含水系统划分的基础上,论证了川西坳上三叠统含水系统隶属于沉积水压系统类型,提出了研究深层水渗流场的原则和方法,并根据计算勾画了研究层水头等值线图和水动力分带图,揭示了深层水的流动特点和规律

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。