不能认识的

Because the obvious advantage of education resource, the university plays amain role in the field of continuing education.

我国普通高校具有学科门类齐全、师资力量雄厚、教育资源丰富的优势，在继续教育领域一直发挥着主导作用，但由于起步较晚，仍然不能完全适应经济发展的需要，与经济发达国家相比差距甚大，突出存在着思想认识不足和制度不完善，物质条件缺乏，管理队伍素质不高等问题，亟需在找准问题的基础上寻求解决的对策。

Their deeds do not allow them to return to their God; For the spirit of harlotry is in them, and they do not recognize the LORD.

他们的行为不能使他们归向天主，因为邪淫的心神潜伏在他们内，致使他们不认识上主。

A scholar I know in Beijing once offhandedly remarked that he had developed self-confidence when learning that he could survive for four years as a teenager on a labor gang during the Cultural Revolution.

我以前还认识一位北京的学者，他说他的自信心是文革当知青时培养起来的，十几岁时在兵团战天斗地连干四年也能熬下来，现在还有什么苦不能吃。

What make the animal run, run away and What makes him tick apart from him prick And the lonelier side of the jealousy stick I don't know, I don't know, I don't know No I don't know, I don't know, I don't know No I don't know, I don't know, I don't know Hell I don't know you any more No, no, no no... Well I don't know if I'm wrong 'Cause she's only just gone Here's to another relationship Bombed by my excellent breed of gamete disease I finished it off with some French wine and cheese La fille danse Quand elle joue avec moi Et je pense que je l'aime des fois Le silence, n'ose pas dis-donc Quand on est ensemble Mettre les mots Sur la petite dodo

什么能使动物奔跑，跑开除开他的刺痛与妒忌更加寂寞的一面，什么能够使他与众不同我不知道，我不知道，我不知道该死的，我都不认识你了我不知我是否错了因为她不过刚刚离去敬有一段被配子疾病的卓越繁殖毁掉的恋爱关系我用一些法国葡萄酒和起司结束它（以下歌词为法语，我不太懂法语，猜着翻的凑合看）那个跳舞的姑娘当我与她一起游戏我想我爱那段时间沉默，不怕谈论任何人当我们在一起将字写在小小的渡渡鸟上

What make the animal run, run away andWhat makes him tick apart from him prickAnd the lonelier side of the jealousy stickI don't know, I don't know, I don't knowNo I don't know, I don't know, I don't knowNo I don't know, I don't know, I don't knowHell I don't know you any moreNo, no, no no...Well I don't know if I'm wrong'Cause she's only just goneHere's to another relationshipBombed by my excellent breed of gamete diseaseI finished it off with some French wine and cheeseLa fille danseQuand elle joue avec moiEt je pense que je l'aime des foisLe silence, n'ose pas dis-doncQuand on est ensembleMettre les motsSur la petite dodo

什么能使动物奔跑，跑开除开他的刺痛与妒忌更加寂寞的一面，什么能够使他与众不同我不知道，我不知道，我不知道该死的，我都不认识你了我不知我是否错了因为她不过刚刚离去敬有一段被配子疾病的卓越繁殖毁掉的恋爱关系我用一些法国葡萄酒和起司结束它（以下歌词为法语，我不太懂法语，猜着翻的凑合看）那个跳舞的姑娘当我与她一起游戏我想我爱那段时间沉默，不怕谈论任何人当我们在一起将字写在小小的渡渡鸟上

Of the five stages deformation, the exact ages of the (2) and (3) were determined by 40Ar/39Ar method as 290 and 259 Ma respectively.2. New results on the metamorphic belts and associated metamorphism of the Xiaopu metamorphic rocksBased on detailed microtextural observations and occurrence of typical metamorphic minerals, five metamorphic belts in the Xiaopu metamorphic rocks are identified. From the north to the south, they are biotite belt, garnet belt, staurolite belt, andalusite belt, and sillimanite belt. I suggested that the metamorphic belts occurred in the Xiaopu area belongs to the high temperature/low pressure series, may have resulted from the later Permian crust extension at ca. 290 Ma.3. I suggest that there may have been a Carboniferous backarc basin along the southern slope of the Harlik Mountain.Detrital Zircon SHRIMP U-Pb dating indicated that the sedimentary age of the Julideneng formation lithic sandstone must be later than late Devonian, most likely is Carboniferous rather than previously thought Precambrian. Analyses on its geologic setting, location of provenance, and sedimentary environment suggest the Carboniferous strata may form in a lagged backarc basin bounded by backarc uplifts.5. Reconstruction of the post-Paleozoic tectonic evolution history of the Harlik MountainThe tectonic evolution of Harlik mountains since the Paleozoic were reconstructed as followings:(1) arc-affinity magmative activities occurred during the middle-Ordovician to early-Silurian;(2) the middle-Silurian to late-Devonian was a back-arc uplift stage;(3) back-arc extension featured the Carboniferous period;(4) post-collisional extension and/then compression during Permian;(5) at the Mesozoic, differential uplift developed; and (6) the late Cenozoic is the intra-continental re-orogen stage.6. Primary estimation of the crust shortening is madeThe folded pre-Mesozoic strata were used to estimate crust shortening along the Harliknanshankou-Koumenzi, Shichengzi-Baishitou, and Qincheng-Xiaopu sections. Their shortening ratios are 16.2%, 19.8%, and 20.1% respectively corresponding crust shortening are 4.3, 9, and 11.3 km.

根据Ar-Ar热年代学研究，精确测定了早二叠世伸展变形和晚二叠世挤压变形的峰期时代分别为290Ma和259Ma.2、提出了关于哈尔里克山南麓小铺一带变质带和变质作用的新认识根据显微观察资料和特征变质矿物的出现，把小铺一带的变质岩由SW向NE方向依次划分为黑云母带、石榴石带、十字石带、红柱石带和矽线石带等变质带；初步确定该区的变质作用属于中温-低压型，变质作用发生的时代为290Ma左右，是该区早二叠世地壳伸展的产物。3、首次提出哈尔里克山南麓在石炭纪可能发育弧后盆地的新观点根据哈尔里克山南麓原"居里得能组"岩屑砂岩的碎屑锆石SHRIMP U-Pb定年，确认这套地层的沉积不早于晚泥盆世，很可能是石炭纪，而不是前人所说的前寒武纪；结合对其区域地质背景、源区位置和沉积环境分析，推测该区石炭纪可能为滞后弧后盆地和弧后隆起区构造背景。4、进一步证明哈尔里克山不发育与岛弧演化相关的泥盆纪岩浆活动根据对代表性闪长岩和花岗岩的锆石SHRIMP年代学研究获得的新资料，结合该区已有相关资料的综合研究，确定哈尔里克山岩浆岩分别形成于奥陶纪-志留纪和石炭纪晚期-二叠纪，不存在泥盆纪的岩浆岩，进而认为该区泥盆纪不属于岛弧环境。5、重建了哈尔里克山古生代以来的地质演化过程根据区域资料以及本次研究所获得的资料，把哈尔里克山古生代以来的构造演化划分中奥陶世-早志留世为岛弧、中志留世-晚泥盆世为弧后区、石炭纪弧后伸展、二叠纪为后碰撞伸展与挤压、中生代差异隆升和晚新生代陆内再造山过程等构造阶段。6、初步估算了哈尔里克山地壳缩短率和缩短量根据前中生代地层褶皱估算的哈尔里克山南山口-口门子、石城子-白石头和沁城-小铺三条剖面的地壳缩短率分别为16.2%、19.8%和20.1%，相应的地壳缩短量分别为4.3km、9km和11.3km。

This is not surprising, given the closer proximity of Pengyang to the Asian inland dust sources; The average content of calcium carbonateis of Pengyang section is not only higher than that of central loess plateau, but also higher the west of Chinese Loess Plateau, which reflected Pengyang loess had been deposited by near Liupanshan\'s substances that contained more calcium carbonateis; The content of diffluent element of 10m depth in the section increased fast, which indicated that the modern eluviation and the leaching depth of loess may be stronger than our guess; The soil growth index can reflect the intensity of soil forming and the climatic changes; The "abrupt chang" of glacial and interglacial period was caused by strong soil-forming processes that enlarged the discrepancy of granularity between loess and paleosol. However, the magnetic susceptibility nearly cannot reflect the existence of S_8 and the magnetic susceptibility of S_7 is highest in the whole section, which is inconsistent with other studies that S_5 has the highest magnetic susceptibility.Thin-section examination shows that the micro-texture of the soil layers is divided into both cementing texture in S_7, S_5 and S_1, and granular texture in all others.

与其它剖面相比，彭阳剖面粒度总体上要比东部的洛川、西安，甚至西部的兰州、新疆东湾要粗；CaCO_3平均含量不仅高于黄土高原中部，也高于高原西部，反映出本剖面富含碳酸盐的六盘山近源沉积起到了很重要的作用；易溶元素含量在剖面10m处快速升高，淀积特征明显，反映出黄土受现代淋溶成土作用影响较大，黄土直立、疏松、多孔特性和高温与多雨组合的气候特点，使得元素淋溶、淀积的强度和深度超出了传统的认识和判断；烧失量与其它指标相比，不仅能区分冰期、间冰期；而且能够区分出次一级的冰阶、间冰阶，有较高的分辨率；土壤发育指数、红度能够反映土壤强度差异，是反映气候波动的较好指标；然而，磁化率不能反映古土壤S_8的存在，且S_7的磁化率在全剖面中最高，这与大多剖面S_5磁化率最高的特点不一致。4。

If be opposite not carefully,this is meant vein sex is impotent try the cent vein leakage that is aimed at different type uses different operation kind to cannot obtain better curative effect, did not add discriminative land in the past alone ligate carries deep vein on the back to fail to obtain ideal curative effect also is at that time the inevitable result of people understanding superficial.

这就意味着如果不仔细对静脉性阳痿加以分型并针对不同类型的静脉漏采用不同的手术方式便不能取得较好疗效，过去不加区别地单独结扎背深静脉未能取得理想疗效也是当时人们认识浮浅的必然结果。

" When will you learn that a father isn t someone you can lean on but someone who rids you of your tendency to lean "?

神甫答：&你什么时候能认识到主不是让你依赖的，而是能帮你摆脱依赖的人？&

Consequently, while it would be unjust to class agnostics, materialists, or pantheists as necessarily also atheists, it cannot be denied that atheism is clearly perceived to be implied in certain phases of all these systems.

因此，尽管这将是不公平的，以一流的不可知论者，唯物论者，或pantheists为一定也是无神论者，但不能否认，无神论是清楚的认识到隐含在某些阶段，所有这些系统。

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。