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The highlight, on the first floor, is a scale model in plaster of a typical Cuban street, the houses fronted with the Greek-revival columns that past sugar wealth bequeathed, the fa ades painted in turn in shocking pink, lime green, toothpaste blue, peach and lemon.

博物馆内一楼有一处显眼的物品,那就是一条用石膏制作而成的一些几何模型,其中包括了一条具有古巴特色的街道,一些前门有着希腊复古风格石柱的房屋…,以及一些依次以显眼的粉色、黄绿色、牙膏蓝、桃色与柠檬色粉刷的各个房屋的正面。

Open again at this moment a moment ago file, warn with respect to occurrence safety, clew grand be banned to use, at this moment we want ordinal alternative " security of tool → grand →", in shooting the dialog box that give, will " grand " safe level setting is " low ", click " affirmatory " save.

这时再打开刚才文件,就出现安全警告,提示宏被禁用,这时我们需依次选择"工具→宏→安全性",在弹出的对话框中,将"宏"安全级设置为"低",并点击"确定"保存。

In general, the tidal flat along Laizhou Bay has typically developed, with the coarsest sediment, namely fine sand on the lower flat, and it grades shoreward into silty sand, sandy silt and silt.

总之,莱州湾的潮滩发育典型,低潮滩的沉积物最粗,为细砂,向陆依次演变为粉砂质砂、砂质粉砂和粉砂,皆呈带状与岸线平行分布。

Familiar location of trauma is shaft of tibia and fibula, shaft of thigh, shaft of ulna and ridius, ankle and foot, chest, knee, coax, pelvis, wrist and hand, shoulder, skull, shoulder bone, spine and elbow in turn. The familiar complication and accompanying trauma is shock, trauma of skull and brain, trauma of chest, trauma of nerve and vessel , fat embolism, trauma of organ in abdomen and trauma of urine system. 3. Emphasizing the treatment before and after the hospital can decrease the mortality and improve the quality of treatment. 4 The effect of early treatment is better than delayed treatment , internal fixation is done in 72h is better than after 72h, which can improve the function and reduce the complication menacing life.

常见的并发症和合并伤依次为:休克、颅脑损伤、胸部损伤、神经血管损伤、脂肪栓塞、腹部脏器损伤和泌尿系损伤。3、多发性骨与关节损伤的治疗以早期内固定效果为好,72h内手术并进行早期功能锻炼的患者远期功能恢第一军医大学2004届硕士学位研究生毕业论文复情况优于超过上述时限手术的患者。4、重视院前急救及院内各科室的急诊救治工作,有效的降低了死亡率,提供了早期处理骨关节损伤的良机。5、早期内固定治疗便于早期开展功能锻炼,可以明显改善伤肢功能,减少了威胁生命的并发症。

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。

In chapter 2, we firstly introduce the model of a discrete-time neural network with generalized input-output function. The model generalizes the input-output function in transiently chaotic neural network to a class of continuous, differentiable and monotone increasing functions. Secondly we study the uniformly asymptotical stability of equilibrium in the non-autonomous model. Finally, several examples and numerical simulations are given to illustrate and reinforce our theories. In chapter 3, we firstly introduce a specific class of discrete-time neural network models with sinusoidal activation function.

在本文的第二章中,首先介绍了一类具有广义输入输出函数的非自治离散神经网络模型,该模型把瞬时混沌神经网络模型中的输入输出函数推广到了一般的单调递增且连续可微的函数;其次,利用Schauder不动点原理和利用Lyapunov函数逆定理依次证明了模型平衡点的存在性和该模型在时变权值下的一致渐近稳定性;最后,对几个具体的例子进行数值模拟,数值模拟的结果更好地说明了我们的结论。

The model generalizes the input-output function in transiently chaotic neural network to a class of continuous, differentiable and monotone increasing functions. Secondly we study the uniformly asymptotical stability of equilibrium in the non-autonomous model. Finally, several examples and numerical simulations are given to illustrate and reinforce our theories. In chapter 3, we firstly introduce a specific class of discrete-time neural network models with sinusoidal activation function.

在本文的第二章中,首先介绍了一类具有广义输入输出函数的非自治离散神经网络模型,该模型把瞬时混沌神经网络模型中的输入输出函数推广到了一般的单调递增且连续可微的函数;其次,利用Schauder不动点原理和利用Lyapunov函数逆定理依次证明了模型平衡点的存在性和在时变权值下的一致渐近稳定性;最后,对几个具体的例子进行数值模拟,数值模拟的结果更好地说明了我们的结论。

The Chitinase of Saccharomyces cerevisiae(CTS1-2) is an Endochitinase which is endogenous in Saccharomyces cerevisiae. Its recognition and slipt site lies in the β-1,4 glucosidic linkage of homopolymer. Included in the amino acid sequence from N-terminal to C-terminal of the Saccharomyces cerevisiae chitinase are signal peptide sequence, catalytic domain, binding domain and a C-terminal shorten region.

酿酒酵母几丁质酶(Chitinase,CTS1-2)是一种来自酿酒酵母的内切几丁质酶,它的酶切位点位于其同聚物内的β-1,4连接的糖苷键,酶蛋白分子结构从N端到C端依次为信号肽、几丁质催化区、几丁质结合区以及一个短的C末端区。

This very moment mood Real own because I very much treasure ourmeeting one another very very much, that has the certain fate, Ireally did not hope because of me the impulse idea, can cause oursentiment for a while to go bad Causes our friendship to change isnot good I really very much blame oneself, because own are the Chinese China'smatter manages again not not well also wants a type foreign countryold person to worry for me, I really very much do not have useful hereme only to be able with you to say again the sound sorry friend ofmine Hoped you can forgive my I since knew I have owed you to be very many always all do not have tobe able also to give you However this I have the difficulty to havein turn said with you, actually again I and you said previous two daysI had thought are very many, should I say with you, but when I makethe phone call for yours time I on regret But or said with you Againhere I hoped you do not blame me, I already very much to regret Triumphant I did not know I this action can let between us nearby thefriendship not be good Triumphant I knew the dissimilarity which weare the heart have cleverness but looked like you before to say,between us the communication really was very difficult to be verydifficult, but was in is difficult I also to hope which country nomatter you were at, perhaps worked I in there all to hope we couldhave the relation Between each other friendship is invariable, knewfinally is good..............

你好凯 此时此刻的心情。真实很很自己因为我很珍惜我们的相遇,那是有一定的缘分的,我真的不希望因为我的一时冲动的想法,会使我们的感情变坏。使我们的友谊变的不好。我真的很责备自己,因为自己是个中国人再中国的事办的不好还要样一个外国老人为我担心,我真的很没有用再这里我只能和您说声对不起我的朋友。希望你能够谅解我一次。我知道我欠你的很多一直以来都没有能够还给你。然而这依次我有困难有和你说,其实再我和你说的前两天我想了很多,我该不该和你说,可是当我把电话打给你的时候我就后悔。可是还是和你说了。再这里我希望你不要怪我,我已经很后悔了。凯我不知道我这次的举动会不会让我们之间的友谊边的不好。凯我知道我们是心有灵犀的但是就象你以前所说的一样,我们之间的沟通实在是很难很难,可是就算是在难我也希望不论你在哪个国家,或是在那里工作我都希望我们能有联系。彼此之间的友谊不变,知道最后好么。。。。。。。。。。。。。。

I am thinking now of a cafe in Venice, a low cliff overlooking the sea near Donegal, a bookstore in Cape Town and Sir John Soane's breakfast room in London.

在《红色》的结尾,在一次海难事故的搜救工作中,三部电影的主角依次出现在银幕上。

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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。