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   shoreline 的翻译结果: 查询用时:0.191秒
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shoreline     
相关语句
  岸线
     Based on the predigested AHP, port shoreline grade evaluation model can be setup.
     建立起港口岸线等级评价的多层次综合评价指标体系后,基于简化的层次分析法(AHP法),确定港口岸线等级评价模型的判定因素和评价指标的权重。
短句来源
     Detection of Lake Shoreline in SAR Image Based on Wavelet
     基于二进小波变换的SAR图像湖岸线提取
短句来源
     APPLICATION OF SHORELINE MODEL ON COASTAL ENGINEERING PROBLEMS
     岸线模型在海岸工程问题中的应用
短句来源
     Port Shoreline Evaluation Model and Its Application
     港口岸线评价模型及其应用
短句来源
     River shoreline space control utilization planning for cities and towns in Guangxi
     广西城镇河道岸线空间控制利用规划的探讨
短句来源
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  海岸线
     Detection of Shoreline in SAR Image Based on Wavelet and GVF Snake Model
     基于小波变换和梯度矢量流Snake模型的ERS-1 SAR图像的海岸线探测
短句来源
     The results showed that: (1) the length of Guangxi shoreline has generally decreased in late 50 years, especially during between 1955 and 1998;
     结果表明:(1)近50年来,广西海岸线总的长度减小,在1955—1998年期间岸线长度呈递减趋势;
短句来源
     The shoreline types fit for bioremediation and the bioremediation technology were discussed.
     探讨了油污染海滩的生物修复技术,以及适合采用该技术的海岸线类型。
短句来源
     In the diffusion model of shoreline fumigation,Lc,He,hf and the correlations between them are the main parameters to decide whether there will be a serious shoreline fumigation.
     在海岸线熏烟扩散模式中,Lc、He与hf的值及其相互关系是决定海岸线熏烟是否发生及其严重程度的主要参数。
短句来源
     Analyses on spatial and temporal changes of Guangxi shoreline based on remote sensing and GIS
     基于遥感和GIS相结合的广西海岸线时空变化特征分析
短句来源
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  滨线
     SHORELINE OF ZABUYE SALT LAKE IN TIBET AND ITS CLIMATIC AND ENVIRONMENTAL SIGNIFICANCE
     西藏扎布耶盐湖滨线及其气候和环境意义
短句来源
     Grain size analysis is done on the sediment of drilling core CBG4a in the marine area of Chengdao, and the authors divide seven sedimentary environments as follows: beach, sand dune near the beach, shoreline of tributary stream outtet of delta, barrier of estuary of the Yellow River Delta,subaqueous prodelta rise of the Yellow River Delta, subaqueous natural leveeand river.
     对埕岛海域CBG4a孔岩芯进行粒度分析 ,划分出海滩、三角洲支流河口滨线、海滩附近沙丘、黄河三角洲河口沙坝、黄河三角洲水下三角洲前缘隆起、水下天然堤、河流等7种沉积环境。
短句来源
     Meanwhile, Longhupao-Da’an terrace west to the deposition is a sedimentary shoreline knick zone, 3 metasequence groups in low-stand tract prograde from old ones to new, and coastal line migrate towards the basin accordingly.
     研究发现研究区低位域地层沉积是在强制性水退背景下形成的,此时其西部的龙虎泡—大安阶地为沉积滨线坡折带,低位域内3个准层序组依次由老到新向盆地进积,滨岸线也相应的向盆地方向迁移。
短句来源
     setting up sequence stratigraphical framework and estimating shoreline onlap cycles in harmony with sedimentary features, was basic to the correlation;
     2 )对比的基础是各盆地建立层序地层格架 ,并估计出与沉积特征和范围尽可能协调的滨线上超旋回 ;
短句来源
     The research results show that the problem about depositional shoreline break for terrigenous sequence along the steep slope zone of fault depressed lacustrine basin can be effectively resolved by using a reference well.
     研究结果表明 ,采用选取参照井的办法 ,可以有效地解决断陷湖盆陡坡带陆相层序地层分析中的“沉积滨线坡折”问题
短句来源
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  湖岸线
     Detection of Lake Shoreline in SAR Image Based on Wavelet
     基于二进小波变换的SAR图像湖岸线提取
短句来源
     The rival channel,lake shoreline and gentle slope are quite important for controlling the delta-front sand-body of lithologic trap in a depression basin.
     在坳陷湖盆,河道、湖岸线和缓坡对有利于岩性圈闭发育的三角洲前缘砂体具有明显的控制作用。
短句来源
     Investigation reveals that the first and second determinants controlling the species richness, numbers of genera and endemic species of lacustrine fishese are respectively the area of the lakes and length of shoreline.
     分析结果显示,控制湖泊鱼类物种丰度、特有种数和属数的关键湖泊环境因子是湖泊面积和湖岸线长度;
短句来源
     Level of lake waves frequently and alternately changes the lake shoreline,resulted in sand-shale interactive deposits in vertical,forming multi sets of oil-bearing assemblages and all kinds of type of lithologic traps formed in sand-shale interactive sedimentation zone of delta front.
     湖平面频繁波动、湖岸线进退交替变化 ,导致纵向上砂泥岩交互沉积 ,形成了多套含油组合 ,在三角洲前缘的砂泥岩交互沉积带形成了多种类型的岩性圈闭 ;
短句来源
     In forepart of Kly the lake shore line popple on east of west slope, source supply is power and the delta is main.
     姚家组沉积早期,湖岸线在西部斜坡东部边缘波动,物源供应相对较强,沉积相以三角洲相对优势。
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      shoreline
    However, the hydrodyamics of the shelf zone differ considerably from those of the open expanses of seas and lakes owing to the steepness of the bottom, the complex structure of the shoreline, the major role of wind waves, and their breaking [1].
          
    For regions of the shelf remote from the shoreline it is also necessary to take into account the interaction of waves with the bottom and with essentially three-dimensional flows.
          
    The mineral field of a complex coastal-marine placer of heavy minerals (CMP), in contrast, reflects practically exclusively the lithodynamic situation within the shoreline zone, including an influence of local factors.
          
    Bioclastic phyto-and zoomorphic limestones occur as wide zones parallel to the shoreline.
          
    Serpukhovian and Bashkirian zoogenic, clastic, and pelitomorphic limestones formed away from the shoreline.
          
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    Tientsin New port, the main port of North China, is situated on the northern part of the subaqueous delta of the Hai-Ho. As the port is faced with silting problem, study of the source of silt is important for formulating measures to cope with the problem. From a detailed study of shoreline changes between New port and the mouth of the Hwangho, together with analysis of grain size, heavy mineral assemblage and clay minerals of sediments of this part of tidal fiats and shallow sea, it seems reasonable to...

    Tientsin New port, the main port of North China, is situated on the northern part of the subaqueous delta of the Hai-Ho. As the port is faced with silting problem, study of the source of silt is important for formulating measures to cope with the problem. From a detailed study of shoreline changes between New port and the mouth of the Hwangho, together with analysis of grain size, heavy mineral assemblage and clay minerals of sediments of this part of tidal fiats and shallow sea, it seems reasonable to conclude that sedi ments causing silting of New port largely come from extensive tidal fiats and shallow sea bottom in the neighborhood of port, i. e. from the subaqueous delta of the Hai-Ho, whereas sediments of the Hwang-Ho mainly go to the deeper part of the Pai-Hai and the southern, western and northern part of the Gulf of Pai-Hai. Thus, although the Hwang-Ho carries a much large amount of sediment, it's influence on silting of New port is only indirect. The formation of the present subaqueous delta of the Hai-Ho dated from the middle 19th century when the outlet of the Hwang-Ho again shifted northwa rd, entering the Pai-Hai. The delta is formed by sediments of the Hai-Ho accumulating around it's original river mouth bar. From the middle 19th century to the early 20th century, there was a rapid growth of the subaqueous delta but afterwards, the pace of growth slowed down. Recently, the building of dikes of New port and the construction of the dam across the mouth of the Hai-Ho have considerably influenced the morphological evolution of the subaqueous delta.

    为研究天津新港回淤泥沙来源问题,本文分析了海河水下三角洲的形成与演变以及渤海湾沿岸地貌与沉积特征。现代海河水下三角洲的粉砂淤泥质滩体是近百年来由海河下泄泥沙形成的。19世纪中叶至20世纪初是三角洲以原河口拦门沙为核心迅速淤长的时期;20世纪初至今,三角洲淤长速度渐缓,但由于海河及其河口地区各种整治工程的影响,三角洲的形态变化很大。近百年来三角洲地貌变化与海河及其河口地区动力泥沙条件有直接关系。通过对海河水下三角洲地貌形成与发育特征的分析,通过渤海湾海岸及水下岸坡地貌和沉积特征的分析,说明天津新港泥沙回淤问题的主要原因是海河水下三角洲地区泥沙的近源活动,港内泥沙主要直接来源于港区周围的广大粉砂淤泥质浅滩。

    Tientsin New port,the main port of North China,is situated on the northern part of the subaqueous delta of the Hai-Ho.As the port is faced with silting problem,study of the source of silt is important for formulating measures to cope with the problem.From a detailed study of shoreline changes between New port and the mouth of the Hwangho,together with analysis of grain size,heavy mineral assemblage and clay minerals of sediments of this part of tidal fiats and shallow sea,it seems reasonable to conclude...

    Tientsin New port,the main port of North China,is situated on the northern part of the subaqueous delta of the Hai-Ho.As the port is faced with silting problem,study of the source of silt is important for formulating measures to cope with the problem.From a detailed study of shoreline changes between New port and the mouth of the Hwangho,together with analysis of grain size,heavy mineral assemblage and clay minerals of sediments of this part of tidal fiats and shallow sea,it seems reasonable to conclude that sedi- ments causing silting of New port largely come from extensive tidal flats and shallow sea bottom in the neighborhood of port,i.e.from the subaqueous delta of the Hai-Ho,whereas sediments of the Hwang-Ho mainly go to the deeper part of the Pai-Hai and the southern,western and northern part of the Gulf of Pai-Hai.Thus,although the Hwang-Ho carries a much large amount of sediment,it's influence on silting of New port is only indirect. The formation of the present subaqueous delta of the Hai-Ho dated from the middle 19th century when the outlet of the Hwang-Ho again shifted northwa rd,entering the Pai-Hai.The delta is formed by sediments of the Hai-Ho accumulating around it's original river mouth bar.From the middle 19th century to the early 20th century,there was a rapid growth of the subaqueous delta but afterwards,the pace of growth slowed down.Recently,the building of dikes of New port and the construction of the dam across the mouth of the Hai-Ho have considerably influenced the morphological evolution of the su- baqueous delta.

    为研究天津新港回淤泥沙来源问题,本文分析了海河水下三角洲的形成与演变以及渤海湾沿岸地貌与沉积特征。现代海河水下三角洲的粉砂淤泥质滩体是近百年来由海河下泄泥沙形成的。19世纪中叶至20世纪初是三角洲以原河口拦门沙为核心迅速淤长的时期;20世纪初至今,三角洲淤长速度渐缓,但由于海河及其河口地区各种整治工程的影响,三角洲的形态变化很大。近百年来三角洲地貌变化与海河及其河口地区动力泥沙条件有直接关系。通过对海河水下三角洲地貌形成与发育特征的分析,通过渤海湾海岸及水下岸坡地貌和沉积特征的分析,说明天津新港泥沙回淤问题的主要原因是海河水下三角洲地区泥沙的近源活动,港内泥涉主要直接来源于港区周围的广大粉砂淤泥质浅滩。

    By using of the accumulative curves of log probability of the particle size analysis, the authors have investigated more than 300 thin sections of the Paleogenic Funing Group and Taizhou Formation in Kiangsu Province, and Changhe Formation in Chekiang Province. It has been found that this method is fairly effective to discriminate the sedimentary environment of ancient sandstone bodies, though it should be verified by other statistical methods of grain size analysis, such as plots of textural paramenters, C....

    By using of the accumulative curves of log probability of the particle size analysis, the authors have investigated more than 300 thin sections of the Paleogenic Funing Group and Taizhou Formation in Kiangsu Province, and Changhe Formation in Chekiang Province. It has been found that this method is fairly effective to discriminate the sedimentary environment of ancient sandstone bodies, though it should be verified by other statistical methods of grain size analysis, such as plots of textural paramenters, C. M. Patterns, as well as by the studies of well log, mineralogy, paleontology and geochemistry, in order to promote the accuracy of interpretation. It is shown from the various plotted graphs that the curves of fluvial sands are dominantly the type curves of two fragments (members), and may be inferred as representing that of deltaic distributary system. Yet there are also curves of three fragments, which may indicate the deposits of torrential rivers. Beach sands have the characteristics of the presence of two saltant components and the absence of suspend component. The constituents of river mouth bar sands and shoreline sands of distributary debouchs are transitional between that of fluvial sands and beach sands. The deposits of levees and crevasse fans consist predominantly of suspend component. It is interesting to note that this method of grain size analysis can, in certain extent, be adopted to interpret the environment of carbonate sands.

    本文用薄片粒度的概率累积曲线分析方法,在与其他相指标相互配合的情况下,试从苏、浙、皖老第三系300多个样品的分析探讨古代河床砂、河口坝砂、天然堤与决口扇砂以及浅滩砂粒度分布的基本特征。并注意到这种粒度分析方法,在一定的条件下,也适用于碳酸盐砂的环境解释。

     
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