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I don't know you. I know the Derek that told me everything.

我不认识你,我认识的Derek什么都告诉我

Her husband seemed to know many of the people who were named, but he replied evasively when asked who they were.

她丈夫好像认识很多被任命的人,但是当别人问他他们是谁时,他推说不认识。

Nurse: Well, I don't know you, but I do know his girlfriend.

好吧,我不认识你,但我认识他的女朋友。

I know when you sit down and when you rise up.

你或许不认识我,我却认识你的一切。

That person understanding my time, I am incognizant

那个人认识我的时候,我不认识他。

She enjoyed trying her French out on Jean-Pierre.

这句话那个法语单词偶不认识有认识的同学请翻译一下

Based on the regional tectonic evolution, combined with the high precision isotopic ages from this paper and other geologists, we have some new acquaintances as follows: 1 There has no Caledonian granite belt distributed in north margin of North China Craton. So, the traditional evolving model of North China Carton, which formed on this idea and the acquaintance about the collision of North China plate and Siberian plate, must be incorrect; 2 The age date show that the earliest magmatic activity began since late-Palaeozoic Permian, which is inconsistent with the previous idea that there were Caledonian and Hercynian active continental margin in the north of North China Craton and in the south Xingkai Massif. 3 the crust and lithosphere were thickened by the subduction and collision of Siberia plate and North China plate during Late Paleozoic. The magma is formed when the crust is heated and melts caused by thickened lithosphere delamination and caused the Asthenosphere upwelling. But only a little basaltic magma erupted, most magma underplate under the bottom of the crust. Thermal energy derived from basaltic magma underplating made the middle and lower crust melt partially and the late Permian-early Triassic granites is formed in large scale.

根据区域构造演化分析,并结合本文及他人高精度同位素年龄,我们对延边花岗岩形成的大地构造环境有了新的认识:1在华北地台北缘并不存在所谓的加里东花岗岩带,因此,建立在此之上的传统的华北地台北缘演化模式及有关西伯利亚板块与华北板块的碰撞拼合的认识也必然是不正确的;2华北地台北缘和兴凯地块南缘不存在加里东期和海西期花岗岩带,表明两地块边缘最早的花岗质岩浆活动始于晚古生代的二叠纪,即不存在传统观点所认为的加里东期或海西期活动陆缘;3晚古生代由于西伯利亚板块与华北板块的俯冲碰撞,致使地壳和岩石圈增厚,导致加厚岩石圈发生拆沉作用,使得软流圈上涌,加热地壳使之熔融形成岩浆,但玄武质岩浆少量喷出地表,大部分底侵于地壳底部,形成下地壳高密度的玄武质底侵层,玄武质岩浆底侵的热能引起中下地壳广泛部分熔融,形成大面积分布的晚二叠世—早三叠世花岗岩。

He smiled as he patted my hand and said,'She doesn't know me, but I

他笑笑,拍拍我的手说:&她不认识我,但我还认识她呀。&

He smiled as he patted my hand and said,she doesn't know me,but I still know who she is.

他笑着拍了拍我的手说,她不认识我,但我一直认识她。

Having only previously visited Jakarta once, in 1999, I did not have any strong impressions of Indonesia. But when I visited Solo in May, I saw pastor Li, whom I had met in 1999. So this time I stayed at his church and visited the 24-hour prayer tower in Gajah Mada, and did some visitation with the local Chinese people.

对印尼的认识不深,只在五年前去过雅加达,但很巧的是五月去Solo时遇到五年前在雅加达认识的牧师,所以这次有机会在雅加达停留,进入Niko牧师的廿四小时祷告塔,也探访认识当地的华人。

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Do you know, i need you to come back

你知道吗,我需要你回来

Yang yinshu、Wang xiangsheng、Li decang,The first discovery of haemaphysalis conicinna.

1〕 杨银书,王祥生,李德昌。安徽省首次发现嗜群血蜱。

Chapter Three: Type classification of DE structure in Sino-Tibetan languages.

第三章汉藏语&的&字结构的类型划分。