小吴尊陆云忠上过北京小伙上非诚勿扰扰吗

非诚勿扰小吴尊丁巨17盏灯视频直播
相关阅读&&&&&&&&
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虹桥小吴尊颓废的声音演唱爱的供养
无聊拿你当猴耍而已
不算多也就几千个!
不过我这个糖儿一个月赚到也不比你少!
或许吧当猴耍!可是当猴子一个月能当几万块钱我很开心啊!
装个好声卡。简单弄个程序。你比他还棒。
山寨的都卖光了啊。 这什么世道啊。 郁闷。
牛逼也别吹破了 几万收入.几万收入也不会呆这样的环境下唱歌了.傻比一个 别丢虹桥人脸了发帖别带虹桥2个字.糖儿头
是不是几万你问那些女主播不就好了!你说小吴尊一个月能收多少钱问一下不!!!
对我是傻逼 我是糖儿头但是你连我这个傻逼都不如&& 你或着真有勇气!
上寨??我笑你见过我的机子??、笑死!
哦。你笑你的。我说我的。呵。
问你啊[婆呢还小吴尊
人家都把你当猴子看 无聊听你耍耍猴戏而已 糖儿头 以后别带虹桥2个字 丢虹桥人的脸
恩恩恩您请继续!
可能吧你想当猴子你当的了吗?、
DJ兄,送他套吧,唱的确实不错,整个调音台给他,唱的绝对好啊
路过而已唱的不错,就是听你唱的同时老感觉,你在看别的什么,某非。。。。。下次分享下,我也想看看那
你拜他做师傅 送他套啊
哈比狗生&&比你唱的都好?
非糖,我和他怎么比,人家可是上过电视的,我只是一个默默无闻的小家伙
我不需要人教了你懂的,人家做歌手我是麦手,怎么比,好比你儿做DJ的我做麦手的我们2个怎么比???
我习惯了!唱歌都要往旁边看看怕旁边有不明飞行物!
天天向上哪一期啊,我去次次
4月份的!!!!
这个傻子又出来卖了、、哎、
o(︶︿︶)o 唉、对个小伙子我只能说、地球已经无法阻止他了、真搞不懂他哪里像吴尊、
恩,好类,我去次次,呵呵,加油啊!
今年4月份木有,去年4月份也木有
&&其实在我心里他一直是喜剧演员!!
&&&&反感西。。
总比有人没有东西出来,麦好吧!
4月份向上吧少年30秒镜头!
好吧我转行去当演员!
反感就不要点吗!
&&&&&& 你能每次发帖不提吴尊么,本来对他还算蛮有感情的,现在。。。。
我和阿容出了作品身边的朋友都同的到、我们不会幼稚到出个什么作品就玩门户上发、我承认我和阿荣都没你那么幼稚、、虹桥门户上聪明人多的是、问问大家、在看看你自己、
这SB已经疯了、不解释、说自己的歌唱的好、长的又像吴尊、我去、就他这样在虹桥也只有那些年过半载的老娘客喜欢、取个ID还叫&&LU&&yun&&zhong&&ku&&&& 我想问他是不是陆云忠酷啊??恶不恶?幼稚不幼稚?还有、我和阿荣不是没作品、是我们觉得一个成熟的男人不会把自己的爱好当成职业来玩的、没人会和你一样、有点什么小东西就在门户上“献宝”幼稚不?还有一点、也是最重要的一点、在虹桥有多少男人会去拍艺术照?就算有、有多少男人会把自己打扮的人不人、鬼不鬼的?
额,我说呢,怎么找不到,我再去次次!
你可以不看我的贴!
其实你唱的很不错。我很喜欢听。。不过。你不懂得谦虚。所以才会被很多人喷
娘娘腔,本姑娘求求你不要再来恶心大众,豹纹?豹纹?MLGBD前天吃的朝阳煲都要吐出来了
声音能不那么恶心么?能不张开你那血盆大口么?
瞎JB呻吟什么玩意儿
qnmlgb&&这是对口型?&&LZ身上散发出那股乡村肥猪流的气息久久没有回过神来&&
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Gzip enabled“小吴尊”丁巨17盏灯反转 刷新新纪录_土豆_高清视频在线观看日托福测验浏览剖析,yiqiniu,美妙旋律第三季51,ben lapps,金钱的魔力课件,陈丽华的前夫,静海一中七仙女,招聘简章,非诚勿扰期,特种部队2qvod,五岁太后,名师讲课视频,乡村里的中国 下载,滑头鬼之孙手机主题,少帅的替身情人,盛世仁杰好看吗,帮帮我爱神在线观看,吴尊篮球火,口腔整形,dnftp技能在哪学,跳蚤市场口号,everytimeyoukissme,吃你吃上瘾,,唐伯虎点秋香2下载,自制wifi信号增强器,明晰谷,,中国教育网高考,衡阳卫校,seqingbobo,softmanager,沙井濠景城,h网大全,独家星劫第二部,平平搭积木ppt
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yiqiniu,美妙旋律第三季51,ben lapps,金钱的魔力课件,陈丽华的前夫,静海一中七仙女,招聘简章,非诚勿扰期,特种部队2qvod,五岁太后,名师讲课视频,乡村里的中国 下载,滑头鬼之孙手机主题,少帅的替身情人,盛世仁杰好看吗,帮帮我爱神在线观看,吴尊篮球火,口腔整形,dnftp技能在哪学,跳蚤市场口号,everytimeyoukissme,吃你吃上瘾,,唐伯虎点秋香2下载,自制wifi信号增强器,明晰谷,,中国教育网高考,衡阳卫校,seqingbobo,softmanager,沙井濠景城,h网大全,独家星劫第二部,平平搭积木ppt,公司邮箱地址大全,jprenti,飞五游戏被查封,国泰君安钱龙金典版,宇丹卡盟,七雄争霸玉龙宝箱,者尼私人影院,星野亚纪快播,金正恩历险记,同事三分亲粤语全集,尚福林 137,索尼爱立信手机大全,浅水洼里的小鱼教学反思,总裁的合约情人,6688商城
此次测验全体难度中等,第一篇和第二篇绝对难度较低,第三篇中的专著名词简单形成考生的浏览停滞,辞汇题根本上都是归于比拟根底的辞汇,在平常的TPO浏览中也有碰着过。三篇文章体裁较常见,辨别是地质类,前史类和社科类。TPO中也有类似操练篇章。
& &第一篇:
体裁分别:地质类文章
首要内容:
bar, 打击扇,delta的造成, upstream和downstream的sediment的比拟。
upstream的局部堆积物可能是鹅卵石之类的大块货色,downstream大多数堆积物是黏土。按理说downstream打击力大,该当是大块的货色才对,起因是downstream的堆积物八成是对upstream的冲蚀效果。
河道的水速率纷歧样,就像气流,冲积扇常常造成新的河流,另有地上河,有些河流一局部在水面之上,一局部在水面之下。
Point bar的话是河道表里侧流速纷歧样,干旱半干旱山区和冰川地域简单造成冲积扇,在湖泊和海滨流速慢的中央会造成delta
大多数的冲积扇面积很广,可是有其中央千年来的冲积扇面积不是很大,这其中央有7个河流,比来有关部分费了很鼎力量整改,想让它不变.
剖析:全体文章布局明晰,比照分明,考生只有捉住各段宗旨便可。门生若是有这方面的布景常识也可帮忙做题。
类似TPO操练举荐:
TPO7- The Geologic History of the Mediterranean
TPO27- The Formation of Volcanic Islands
关联文章:
Earth’s surface is not made up of a single sheet of rock that forms a crust but rather a number of “tectonic plates” that fit closely, like the pieces of a giant jigsaw puzzle. Some plates carry islands or continents others form the seafloor. All are slowly moving because the plates float on a denser semi-liquid mantle, the layer between the crust and Earth’s core. The plates have edges that are spreading ridges (where two plates are moving apart and new seafloor is being created), subduction zones (where two plates collide and one plunges beneath the other), or transform faults (where two plates neither converge nor diverge but merely move past one another). It is at the boundaries between plates that most of Earth’s volcanism and earthquake activity occur.
Generally speaking, the interiors of plates are geologically uneventful. However, there are exceptions. A glance at a map of the Pacific Ocean reveals that there are many islands far out at sea that are actually volcanoes----many no longer active, some overgrown with coral----that originated from activity at points in the interior of the Pacific Plate that forms the Pacific seafloor.
How can volcanic activity occur so far from a plate boundary? The Hawaiian Islands provide a very instructive answer. Like many other island groups, they form a chain. The Hawaiian Islands Chain extends northwest from the island of Hawaii. In the 1840s American geologist James Daly observed that the different Hawaii islands seem to share a similar geologic evolution but are progressively more eroded, and therefore probable older, toward the northwest. Then in 1963, in the early days of the development of the theory of plate tectonics. Canadian geophysicist Tuzo Wilson realized that this age progression could result if the islands were formed on a surface plate moving over a fixed volcanic source in the interior. Wilson suggested that the long chain of volcanoes stretching northwest from Hawaii is simply the surface expression of a long-lived volcanic source located beneath the tectonic plate in the mantle. Today’s most northwest island would have been the first to form. They as the plate moved slowly northwest, new volcanic islands would have forms as the plate moved over the volcanic source. The most recent island, Hawaii, would be at the end of the chain and is now over the volcanic source.
Although this idea was not immediately accepted, the dating of lavas in the Hawaii (and other) chains showed that their ages increase away from the presently active volcano, just as Daly had suggested. Wilson’s analysis of these data is now a central part of plate tectonics. Most volcanoes that occur in the interiors of plates are believed to be produced by mantle plumes, columns of molten rock that rise from deep within the mantle. A volcano remains an active “hot spot” as long as it is over the plume. The plumes apparently originate at great depths, perhaps as deep as the boundary between the core and the mantle, and many have been active for a very long time. The oldest volcanoes in the Hawaii hot-spot trail have ages close to 80 million years. Other islands, including Tahiti and Easter Islands in the pacific, Reunion and Mauritius in the India Ocean, and indeed most of the large islands in the world’s oceans, owe their existence to mantle plumes.
The oceanic volcanic islands and their hot-spot trails are thus especially useful for geologist because they record the past locations of the plate over a fixed source. They therefore permit the reconstruction of the process of seafloor spreading, and consequently of the geography of continents and of ocean basins in the past. For example, given the current position of the Pacific Plate, Hawaii is above the Pacific Ocean hot spot. So the position of The Pacific Plate 50 million years ago can be determined by moving it such that a 50-million-year-oil volcano in the hot-spot trail sits at the location of Hawaii today. However because the ocean basins really are short-lived features on geologic times scale, reconstruction the world’s geography by backtracking along the hot-spot trail works only for the last 5 percent or so of geologic time.
体裁分别:前史类文章
首要内容:
非洲农牧业的迁移。
非洲雨水充分的中央,一开端不种田,厥后一其中央的人引进了一种动物,而后他们开端种田。厥后干旱了,往东边高原去了,雨季的时分狩猎,旱季就种田。
牧业的话养牛要克制许多前提。农业的话是先开垦一片地盘,而后地盘没有肥力了就摈弃再去下一其中央,然而这类农业形式也是需求许多技术不是那末简略粗犷的。
就文章体裁而言,是考生绝对不是很生疏的论题,就浏览而言不存在太大的成绩,放善意态便可。
类似TPO操练举荐:
TPO21- The Origins of Agriculture
TPO14- Pastoralism in Ancient Inner Eurasia
关联文章:
Pastoralism is a lifestyle in which economic activity is based primarily on livestock. Archaeological evidence suggests that by 3000 B.C., and perhaps even earlier, there had emerged on the steppes of Inner Eurasia the distinctive types of pastoralism that were to dominate the region"s history for several millennia. Here, the horse was already becoming the animal of prestige in many regions, though sheep, goats, and cattle could also play a vital role. It is the use of horses for transportation and warfare that explains why Inner Eurasian pastoralism proved the most mobile and the most militaristic of all major forms of pastoralism. The emergence and spread of pastoralism had a profound impact on the history of Inner Eurasia, and also, indirectly, on the parts of Asia and Europe just outside this area. In particular, pastoralism favors a mobile lifestyle, and this mobility helps to explain the impact of pastoralist societies on this part of the world.
The mobility of pastoralist societies reflects their dependence on animal-based foods. While agriculturalists rely on domesticated plants, pastoralists rely on domesticated animals. As a result, pastoralists, like carnivores in general, occupy a higher position on the food chain. All else being equal, this means they must exploit larger areas of land than do agriculturalists to secure the same amount of food, clothing, and other necessities. So pastoralism is a more extensive lifeway than farming is. However, the larger the terrain used to support a group, the harder it is to exploit that terrain while remaining in one place. So, basic ecological principles imply a strong tendency within pastoralist lifeways toward nomadism (a mobile lifestyle). As the archaeologist Roger Cribb puts it, “The greater the degree of pastoralism, the stronger the tendency toward nomadism.” A modern Turkic nomad interviewed by Cribb commented: "The more animals you have, the farther you have to move."
Nomadism has further consequences. It means that pastoralist societies occupy and can influence very large territories. This is particularly true of the horse pastoralism that emerged in the Inner Eurasian steppes, for this was the most mobile of all major forms of pastoralism. So, it is no accident that with the appearance of pastoralist societies there appear large areas that share similar cultural, ecological, and even linguistic features. By the late fourth millennium B.C., there is already evidence of large culture zones reaching from Eastern Europe to the western borders of Mongolia. Perhaps the most striking sign of mobility is the fact that by the third millennium B.C., most pastoralists in this huge region spoke related languages ancestral to the modern Indo-European languages. The remarkable mobility and range of pastoral societies explain, in part, why so many linguists have argued that the Indo-European languages began their astonishing expansionist career not among farmers in Anatolia (present-day Turkey), but among early pastoralists from Inner Eurasia. Such theories imply that the Indo-European languages evolved not in Neolithic (10,000 to 3,000 B.C.) Anatolia, but among the foraging communities of the cultures in the region of the Don and Dnieper rivers, which took up stock breeding and began to exploit the neighboring steppes.
Nomadism also subjects pastoralist communities to strict rules of portability. If you are constantly on the move, you cannot afford to accumulate large material surpluses. Such rules limit variations in accumulated material goods between pastoralist households (though they may also encourage a taste for portable goods of high value such as silks or jewelry). So, by and large, nomadism implies a high degree of self-sufficiency and inhibits the appearance of an extensive division of labor. Inequalities of wealth and rank certainly exist, and have probably existed in most pastoralist societies, but except in periods of military conquest, they are normally too slight to generate the stable, hereditary hierarchies that are usually implied by the use of the term class. Inequalities of gender have also existed in pastoralist societies, but they seem to have been softened by the absence of steep hierarchies of wealth in most communities, and also by the requirement that women acquire most of the skills of men, including, often, their military skills.
体裁分别: 社科类文章
首要内容:
是一个地域社会文明的变化。
发觉了许多东西,举例。。。,然而没有发觉罐子。他们跟之宿世活在这里的人纷歧样。生计规模变得很大,有些屋子能够住一年或半年。 他们吃肉,肉类供给许多的必需的盐,他们也更需求盐,为了保留肉。他们会用点缀物,而后这推进了身份和阶层开展,社会状态愈加杂乱。
就全体的文章布局来看,考生可经过浏览对应的TS句来理解段落的粗心,比拟照拟简单掌控,标题难度也不高,根本上均能够从译文中找到对应的资讯点。
类似TPO操练举荐:
TPO5— The Origin of the Pacific Island People
TPO 9-Colonizing the Americas via the Northwest Coast
关联文章:
The greater Pacific region, traditionally called Oceania, consists of three cultural areas: Melanesia, Micronesia, and Polynesia. Melanesia, in the southwest Pacific, contains the large islands of New Guinea, the Solomons, Vanuatu, and New Caledonia. Micronesia, the area north of Melanesia, consists primarily of small scattered islands. Polynesia is the central Pacific area in the great triangle defined by Hawaii, Easter Island, and New Zealand. Before the arrival of Europeans, the islands in the two largest cultural areas, Polynesia and Micronesia, together contained a population estimated at 700,000.
Speculation on the origin of these Pacific islanders began as soon as outsiders encountered them, in the absence of solid linguistic, archaeological, and biological data, many fanciful and mutually exclusive theories were devised. Pacific islanders are variously thought to have come from North America, South America, Egypt, Israel, and India, as well as Southeast Asia. Many older theories implicitly deprecated the navigational abilities and overall cultural creativity of the Pacific islanders. For example, British anthropologists G. Elliot Smith and W. J. Perry assumed that only Egyptians would have been skilled enough to navigate and colonize the Pacific. They inferred that the Egyptians even crossed the Pacific to found the great civilizations of the New World (North and South America). In 1947 Norwegian adventurer Thor Heyerdahl drifted on a balsa-log raft westward with the winds and currents across the Pacific from South America to prove his theory that Pacific islanders were Native Americans (also called American Indians). Later Heyerdahl suggested that the Pacific was peopled by three migrations: by Native Americans from the Pacific Northwest of North America drifting to Hawaii, by Peruvians drifting to Easter Island, and by Melanesians. In 1969 he crossed the Atlantic in an Egyptian-style reed boat to prove Egyptian influences in the Americas. Contrary to these theorists, the overwhelming evidence of physical anthropology, linguistics, and archaeology shows that the Pacific islanders came from Southeast Asia and were skilled enough as navigators to sail against the prevailing winds and currents.
The basic cultural requirements for the successful colonization of the Pacific islands include the appropriate boat-building, sailing, and navigation skills to get to the islands in the first place, domesticated plants and gardening skills suited to often marginal conditions, and a varied inventory of fishing implements and techniques. It is now generally believed that these prerequisites originated with peoples speaking Austronesian languages (a group of several hundred related languages) and began to emerge in Southeast Asia by about 5000 B.C.E. The culture of that time, based on archaeology and linguistic reconstruction, is assumed to have had a broad inventory of cultivated plants including taro, yarns, banana, sugarcane, breadfruit, coconut, sago, and rice. Just as important, the culture also possessed the basic foundation for an effective maritime adaptation, including outrigger canoes and a variety of fishing techniques that could be effective for overseas voyaging.
Contrary to the arguments of some that much of the pacific was settled by Polynesians accidentally marooned after being lost and adrift, it seems reasonable that this feat was accomplished by deliberate colonization expeditions that set out fully stocked with food and domesticated plants and animals. Detailed studies of the winds and currents using computer simulations suggest that drifting canoes would have been a most unlikely means of colonizing the Pacific. These expeditions were likely driven by population growth and political dynamics on the home islands, as well as the challenge and excitement of exploring unknown waters.&
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