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the Middle Ages相关的网络例句

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We define the ADR and the ADRcompensation in the theory research. The paper goes into detail about the ADR theory basis andthe responsibility constitution of other countries and provides the theory basis in order to make itclear why the victims should get the compensation and who should undertake the responsibility.(3)According to the analysis of the data statistical and the investigation, most reports come from themedical institutions while the reports from the production and operation enterprises are extremelyfew, only making up 1%. The speakers are mostly doctors. The serious ADR is about 2% andoccur at different ages. 50 -year-old middle-aged persons and old persons suffer from the ADReasily. In those reports, the ADR caused by using the one drug is about 90%; the ADR caused bythe anti-infection medicine ranks first due to using it wide in clinical medicine and applyingunreasonably. The intravenous injection easily causes the ADR.

对各国药品不良反应损害补偿的理论基础和责任构成进行阐述,为解决为什么要对药品不良反应受害者进行补偿、由谁承担责任提供了理论依据。3、我国药品不良反应现状研究方面,药品不良反应数据统计分析调查,发现报告主要来源于医疗机构,生产和经营企业报告数量极少,企业的报告数只占总数的1%,报告人都是以医生为主,严重不良反应发生的比例占药品不良反应报告总数的2%左右,不同年龄段都有药品不良反应发生,其中年龄大于50岁的中老年人发生的几率最大,在药品不良反应报告总数中,主要是使用一种药品的情形,占90%左右,抗感染药物占各类药物的首位,这与抗感染药物在临床广泛及不合理应用有关,静脉给药一直高居引起药品不良反应给药途径之首。

The Pb-Pb isochron of metamorphic argillite in Shuangqiaoshan Group is 1 490±68 Ma, while the Nd mode ages of Zhanggongshan Group, Shuangqiaoshan Group, Chenglang Group and Xiushui Group are 1.57 Ga, 1.89 Ga, 1.77 Ga, 1.60 Ga,respectively, less than 1.6-1.9 Ga, which suggest that they formed in Middle Proterozoic Subera.

研究结果还显示,双桥山群变质泥质岩的Pb-Pb等时线年龄为(1 490±68)Ma,而障公山群、双桥山群、程浪群和修水群的钕模式年龄分别为1.57 Ga、1.89Ga、1.77Ga和1.60 Ga,均分布在1.5~1.9 Ga之间,表明这些地层的形成年龄应小于1.9 Ga,是中—晚元古代的产物,同时表明扬子古陆南缘存在古元古代的基底。

It is because that the students of different ages have great difference in intellectual structure, body and mind character , lifer exprience ., knowledge-level ., capacity of understanding , So project-learning curriculum in Primary school and Junior middle school cant copy the model of Senior middle school curriculum , and should open a suitable curriculum according to the body and mind character of students in Primary school and Junior middle school, although the National Ministry of Education have promulgated the project-learning curriculum in Senior mddle school.

因此,尽管国家教育部已经颁布了高中的研究性学习课程,但小学和初中的研究性学习课程不照搬高中课程的模式,而因根据其身心特点设置与之相适应的课程。

It is because that the students of different ages have great difference in intellectual structure, body and mind character , lifer exprience ., knowledge-level ., capacity of understanding , So project-learning curriculum in Primary school and Junior middle school cant copy the model of Senior middle school curriculum , and should open a suitable curriculum according to the body and mind character of students in Primary school and Junior middle school,although the National Ministry of Education have promulgated the project-learningcurriculum in Senior mddle school.

因此,尽管国家教育部已经颁布了高中的研究性学习课程,但小学和初中的研究性学习课程不照搬高中课程的模式,而因根据其身心特点设置与之相适应的课程。

This middle view is but a weak attempt at saving something of the full Solomonic authorship affirmed in earlier ages.

这中间的观点是一个薄弱的企图,但在一些省的充分肯定Solomonic作者在较早年龄。

But on the other hand, middle school students, who are in the age of acute changes and rapid development in body and mind, are curious and attentive about the changes and development of the society, sensitive and treasonous in thoughts, and the attitude and feelings of the students in different ages in learning politics are quite different.

因此,在思想政治课教学中,必须重视对学生学习能力的培养。

On the basis of volcanological study,here we present thirty one K-Ar ages of basaltic rocks and two 14C ages of coke and peat. The history of LGV Quartenary activities can be divided into three main periods, namely Xiaoyishan Period (Early Pleistocene:2.15~0.75Ma), Longang Period (Middle-Late Pleistocene::0.68~0.05Ma) and Jinglongdingzi Period Holocene:1600~1500a.

根据31个火山岩K-Ar年龄和2个炭化木与泥炭层的14C年龄,将龙岗第四纪火山活动分为三期:小椅山期(早更新世:2.15~0.75Ma)、龙岗期(中-晚更新世:0.68~0.05Ma)和金龙顶子期(全新世:1600~1500a。

Based on isotopic ages and the cycle of magamtism, the ages of Yanbian granites can be subdivided into five periods:①late Permian granites (260-245Ma), the typical plutons are Liukesong and Liangbing plutons, and the main rock type include diorite-monzonitic-K syenogranites;②Triassic granites (225-200Ma), the typical plutons are Sandaogou, Chunyang, Qishiergedingzi, Dahuanggou, Naozhi, and Qinglinzi plutons, the main rock type include quartz dioritesgranodiorites-monzonitic-alkali granites;③early Jurassic granites (190-180Ma), which composed of quartz diorites-granodiorites - monzonitic ,and the typical plutons are Shimen, Miantian, Daxinggou and Yushuchuan rock;④Middle-Late Jurassic (170-150Ma), which composed of granodiorites- monzonitic- garnet-bearing muscovite granites, the typical plutons are Huangniling, Weizigou, Loutuoshan and Dongqing rock;⑤early Cretaceous (about 130Ma), the typical pluton is Zhongping pluton, and its rock type is paulite diorite.

另外,根据同位素年龄和岩石组合并考虑到岩浆的旋回性,将延边显生宙花岗岩进一步划分为五个期次:1。晚二叠世(260-245Ma),代表性岩体为六棵松和亮兵,主体岩性为辉石闪长岩、二长花岗岩和钾长花岗岩;2。三叠世(225-200Ma),代表性岩体为三道沟、春阳、七十二个顶子、大荒沟、闹枝、青林子,岩石组合为石英闪长岩—花岗闪长岩—二长花岗岩—碱长花岗岩,以花岗闪长岩和二长花岗岩为主;3。早侏罗世(190-180Ma),石英闪长岩—花岗闪长岩—二长花岗岩组合,主体岩性为花岗闪长岩,代表性岩体有石门、棉田、大兴沟、榆树川等;4。中侏罗世(170-150Ma),主体岩性为花岗闪长岩和含石榴石花岗岩,代表性岩体有黄泥岭、苇子沟、骆驼山、东清5。

The2 0 th century was the third high-tlide of researches on paradox in the west following the ancient Greek and Middle Ages studies.Which can be divided into three periods,the first of which was from190 1to the1930 s when Russel discovered it,mainly emphasizing collective paradoxical studies.The second one was from the1940 s to the mid-1970 s,it m ainly stressed the semantic para- doxical studies.

20世纪西方悖论研究是继古希腊和中世纪之后出现的第三次悖论研究的高潮时期,可划分为三个阶段:1 90 1年罗素悖论发现至 30年代末为第一阶段,主要以集合论悖论研究为重点;4 0年代初至 70年代中叶为第二阶段,逐渐转移到以语义悖论研究为重点;70年代中叶至 2 0世纪末为第三阶段,回归到自然语言,在语形、语义、语用的统一中研究悖论问题。

In the later Middle Ages, when the black monks were giving less time to agriculture, the Cistercians reestablished the old order of things; and even today such monasteries as La Trappe de Staoueli in northern Africa, or New Nursia in western Australia do identically the same work as was done by the monks a thousand years ago.

在后来的中世纪,当黑色的和尚被给予的时间更少,农业,熙笃会重新确立了旧秩序的事情;即使在今天,这样的寺庙,像过La Trappe ;德斯塔韦利在非洲北部,或新努西亚在澳大利亚西部的做相同的同工作做了和尚一千多年前。

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