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  group area
     PRELIMINARY ANALYSIS OF GRAVITY DATA ON THE SOUTH TUVALU REEF GROUP AREA
     南图瓦卢礁群区重力资料的初步分析
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     Construction techniques for a railway tunnel passing through karst group area
     铁路隧道穿越岩溶群区施工控制技术研究
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     The paper describes the construction techniques on the section from DK215+650 to DK216+105, where group of karsts are encountered, for Bantao tunnel on Yu (Chongqing) Huai (Huaihua) railway. In order to guarantee the construction time limit for this project, a bypass adit was excavated to make a detour of the karst group area, it was connected with main tunnel by a transverse gallery.
     文章以渝(重庆)怀(怀化)铁路板桃隧道为工程背景,阐述了该隧道穿越DK215+650~DK216+105段岩溶群区的施工技术。
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  “群区”译为未确定词的双语例句
     Translocations involving a breakpoint cluster region BCR of the mixed-lineage leukemia MLL gene at chromosome band 11q23 are the most common molecular abnormalities in acute leukemias of infants and acute leukemias related to chemotherapy with DNA topoisomerase Ⅱ inhibitors.
     染色体11q23的混合谱系白血病(MLL)基因的断裂点簇集群区(BCR)的转位,可引起婴儿急性白血病及与DNA拓扑异构酶Ⅱ抑制剂的生化治疗法相关的白血病。
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     ③The construction of digital city in urban agglomeration, which promotes the urban modernization.
     ③城市群区内数码城市的建立 ,促进了城市现代化。
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     THE DEVELOPMENT TREND OF URBAN AGGLOMERATION IN SHANGHAI-NANJING-HANGZHOU AREA
     沪宁杭城市群区发展趋势探讨
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     The Development of Urban Group in the Information Society
     信息环境下城市群区的发展
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     The islands region can be subdivided into three sub regions again according to the development degree of tidal channels:Ⅲ 1 northern region of the Zhoushan Islands,Ⅲ 2 southern region of the Zhoushan Islands,and Ⅲ 3 region south of Zhoushan Islands.
     其中岛群区依据潮汐通道的发育程度又划分为 3个亚区 : 1 舟山群岛北区、 2 舟山群岛南区、 3南部岛群区
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     The Effect of a Group of Forest Within a Farmland Region on the Runoff
     农对径流的影响
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     On the Building up of the Urban Agglomeration in theMiddle Reaches of the Yangtze River
     论建设长江中游城市
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     HOMOMORPH-GROUP
     态
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     Group B contains T.
     B由T .
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     necking down region;
     颈缩 ;
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  group area
The aggregation numbers and radii of micelles, the hydrophilic group area, and the parameters of critical compaction of micelles are calculated from the data on fluorescence quenching by hexadecylpyridinium bromide.
      
The modification implies that the system is free to choose an optimal head group area and an optimal arrangement of the surfactant molecules in the interface as a function of bulk concentration.
      
The fraction of the total sunspot group area that is found in the leading spots is discussed as a parameter that can be useful in studying the dynamics of sunspot groups.
      
During the tundra group decrease in the first half of the century boreal group area also decreased while temperate group area increased.
      
Education welfare action zones were selected in low-income group area in the metropolis.
      
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It is difficult to establish the stratigraphic sequences in the area of low grade rock. This paper introduces a method for a solution. Firstly, we should judge stratigraphic younging up, structural facing, vergence and determine tectonic style. Secondly stratigraphic sequence can be established on specific feature of the tectonic style. This has been used and correlated by author in analysising sedimentary system and mapping upper Proterozoic Huashan Group in Dahong-shan Mountain, Hubei provence.

本文结合实例叙述了一种浅变质岩区地层层序建立和检验的方法.在浅变质岩区建立地层层序,首先应充分搜集各种原生和变形结构要素,鉴定岩层的变新方向、构造面向、构造降向,进行构造组合和应变分析,确定构造样式群特征.其次,依构造样式群特征,建立地层层序,划分地层.最后本文通过对湖北大洪山花山群区测填图、沉积环境与地层成因分析检验了所建立的地层层序.

After injecting the posterior pituitery of the albino rats with cholera-toxin

在大鼠垂体后叶内注入霍乱毒素结合辣根过氧化物酶后,在终纹床核群区发现一些逆行标记细胞。根据最近对于终纹床核群的细胞构筑学的研究,本文分析了其逆行标记细胞的分布。在终纹床核群的前腹区内,在纹旁核内有少量树突,核周有少量细胞;有一些散在的大细胞核神经元;腹侧核内也有一些标记细胞。在终纹床核群后部的背侧半附近,有若干比较明显的标记细胞群,包括前穹窿核、内侧背副细胞群、外侧背副细胞群及室间孔下群。这些细胞群紧靠终纹床核群,却难以归入终纹床核群本身。但其树突往往伸入至终纹床核后部的主核或束间核内,与终纹床核具有共同的传入来源。还有少量细胞非恒定地散在于终纹床核群各处。

According to geological tectonics and seismic activites this paper devided North China ( 30°- 45°N, 105 - 130°E) into four areas . We analized the Nouth China earthquake catalogue from 1970 to 1986 (from 1965 to 1986 for Hua Bei, the North China, plain region) and identified forty- two bursts of aftershock. Seven of them occurred in aftershock regions of strong earthquakes and seventeen of them in the seismic swarm regions. The relation between strong earthquakes with the remaining eighteen bursts of aftershocks...

According to geological tectonics and seismic activites this paper devided North China ( 30°- 45°N, 105 - 130°E) into four areas . We analized the Nouth China earthquake catalogue from 1970 to 1986 (from 1965 to 1986 for Hua Bei, the North China, plain region) and identified forty- two bursts of aftershock. Seven of them occurred in aftershock regions of strong earthquakes and seventeen of them in the seismic swarm regions. The relation between strong earthquakes with the remaining eighteen bursts of aftershocks has been studied and tested statistically in this paper. The result of statistical testing show that the random probability p of coincidence of bursts of aftershock with subsqeuent strong earthquakes is less than six percent. By Xu's R scoring method the efficacy of predicating strong earthquake from bursts of aftershock is estimated qreater than 39 percent .Following the method proposed in the paper we analyzed the earhtquake catalogue of China from 1987 to 1988-6 The results show that there was only one brust of aftershock occurred on Jan. 6,1988 with M=3.6 in Xiuyan of Northeast China. It implicates that a potential earthquake with Ms≥ 5 might occur in one year afterwards in the region of Northeast China. Actually on Feb.25,1988 an earthquate with Ms= 5.3 occurred in Zhangwu of Northeast China. Another example is Datong-Yanggao shock on October -18, 1989 which is a burst of aftershock. Three hours after an expected shock with M=6.l took place in the same area. Two examples above have been tested in practical predication and this shows that bursts of aftershock are significant in predicating strong earthquakes.

本文按地质构造和地震活动水平,分大华北地区成四个子域.并分析了大华北地区1970—1986年地震目录(其中华北平原子域地震目录为1965—1986年)检测得到爆发余震42次.其中7次发生在强震的余震区,17次发生在震群区.研究其余的18次爆发余震与强震关系,并进行统计检验.结果表明:这18次爆发余震与其后强震发生的随机相遇概率小于6%.用许氏 R 值评分方法估算的爆发余震预报强震的效能大于39%.按照本文给出判定爆发余震的参数,对1987—1988年地震目录进行了外推检验预测.1987—1988年仅有一个爆发余震,即1988年1月6日东北岫岩3.6级地震.它预示1988年1月—1989年1月,东北地区可能有 M_s≥5.0地震.实际情况是在1988年2月25日,在东北章武地区发生了一次 M_s=5.3地震.另一个实例是在1989年10月18日山西大同—阳高地区发生了一次爆发余震,其后3小时在同一地区也发生了预计的 M_s=6.1地震.以上两例都在实际预报中验证了.爆发余震可能具有一定的预报中强震的能力.

 
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