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   构造等高线 的翻译结果: 查询用时:0.238秒
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构造等高线
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  structural contour
     So the reservoir pinch-out boundary is fixed on the 10m isopach of carboniferous residuum thickness. (Based on drilling data and interpretation of polarity, amplitude and moveout of seismic reflector in Permian bottom. ) On the basis of carboniferous structures and their structural contour lines,it is forecasted that there are 48 kinds of carboniferous stratigraphic-structural combination traps which is divided into & types in Eastern Sichuan.
     以石炭系残厚10m等厚线(据二叠系底界地震反射层的极性、振幅和时差 等信息结合地面和井下资料确定)作为储层的尖灭边界,据其展布与石炭系构造和构造等高线相配置的关系,预测出川东 石炭系地层-构造复合圈闭有8种类型48个圈闭,已探成功率达65%,还有多半圈闭未探,前景乐观。
短句来源
     As to lithologic reservoir characterized by being generated and reservoired indigenously,the upwarping pinch-out sandbodies are nearly perpendicular to the structural contour lines of nose setting,leading to the formation of large area sandstone upwarping pinch-out or lateral margin upwarping pinch-out lithologic oil/gas reservoirs.
     对于自生自储型的岩性油气藏来讲,上翘尖灭砂体与鼻状构造背景的构造等高线近于正交,形成了大面积砂岩上翘尖灭或侧缘上翘尖灭岩性油气藏。
短句来源
  “构造等高线”译为未确定词的双语例句
     Three Arithmetics on Constructing the Protraction of Contour
     关于构造等高线绘制的3种方法
短句来源
     The superimposed basins have three main migration\|accumulation models: ①radial migration and annular accumulation model, such as circle\|hero mount accumulation belt of western Qaidam basin, in which the hydrocarbon migration direction is perpendicular to the contour lines of the basin;
     多期叠合盆地有 3种基本油气运聚模式 :①放射状运移、环状聚集模式 ,以柴达木盆地西部环英雄岭构造带为代表 ,油气运移方向垂直于构造等高线的方向 ;
短句来源
     The bedded permeable layer supply oil is controlled by structural hights,the migration paths are usually the counter lines of vertical structures,and oil migrates towards the height of noze structure along the noze bridg.
     层状渗透层供油受构造高点控制 ,运移路径一般为垂直构造等高线沿鼻状构造的鼻梁向构造高点运移。
短句来源
  相似匹配句对
     “L-STRUCTURE”FOR FUZZY SET IN A LINEAR SPACE
     L—构造
短句来源
     The X.
     在构造 X.
短句来源
     Structural Analysis of Coal-Floor Contour Map
     煤层底板等高线图上的构造分析
短句来源
     Three Arithmetics on Constructing the Protraction of Contour
     关于构造等高线绘制的3种方法
短句来源
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  structure contour
On the basis of MTS and DSS data in and near Tianshui region, the deep structure contour of the region was expounded.
      
Where exploration involves the application of polynomial trend analysis to structure contour maps in the search for petroleum and natural gas, standard analysis of variance tests may not indicate the best exploration maps.
      
Reflection-time measurements have been converted to depth values, corrected for postdepositional tilting, and portrayed as structure contour maps, perspective "fish-net" diagrams, and isopach maps prepared by computer.
      
Several extensive `Hinge faults' that abut at high angles to the arc orientation, are inferred from aninterpretation of the structure contour map.
      
In structure/contour matching methods, outliers are often a significant source of error.
      
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  structural contour
Structural contour maps applied in the analysis of double fold structures
      
The application of structural contour maps based on data obtained from surface mapping is outlined and the limits and the advantages of the method when applied to double fold structures are discussed.
      
The structural contour map of the Moho prepared from the present data set, indicates the crustal thickness of about 37 km in the western margin of the basin, thinning to about 28 km in the east with an upwarp in the Moho boundary.
      
Structural contour map of the base of Cenozoic rocks in the Sevier Desert.
      
Structural contour map on top of the proposed injection zone.
      
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On the basis of precursory works, the author suggests a method to draw the foldtransverse section in undulated relief. As compared with the drawing method intro-duced by Donal M. Ragan, the present method has more extensive application andmore simple procedure. The author also suggests two methods to draw a fold longi-tudinal section and a top (bottom) section, by means of which it is possible to quantitatively study the fold forms comprehensively. At the same time, the author suggeststhe drawing methods to...

On the basis of precursory works, the author suggests a method to draw the foldtransverse section in undulated relief. As compared with the drawing method intro-duced by Donal M. Ragan, the present method has more extensive application andmore simple procedure. The author also suggests two methods to draw a fold longi-tudinal section and a top (bottom) section, by means of which it is possible to quantitatively study the fold forms comprehensively. At the same time, the author suggeststhe drawing methods to obtain fault fotal slip in undulated relief, as well as theform of fault plane, total slip and tri-directional fold sections on a structural con.tours map.

构造地质学的基础工作是研究褶皱与断层的形态。以往对于地质构造形态的研究,主要是定性地描述;或者在地形平坦的条件下,求褶皱的横截面与断层的总滑距。近年来,D.M.拉根所著《构造地质学——几何方法导论》一书,全面介绍了用几何方法研究构造形态的方法。他在书中介绍了在地形起伏情况下作褶皱横截面图的方法,但在某些情况下应用有局限性,作图方法较为复杂。书中没有介绍在地形起伏情况下如何求断层总滑距的方法。现在本文作者在前人工作的基础上,提出另一种在地形起伏情况下作褶皱横截面图的方法,这种方法在较少情况下应用有局限性,作图方法较为简便。作者在此同时提出了作褶皱纵截面图与顶(底)截面图的二种方法,以便能够全面定量地研究褶皱的形态。作者在此还提出了在地形起伏情况下求断层总滑距的方法,以及在构造等高线图上求断层面形态。总滑距与褶皱三个方向截面图的方法。

Building structure model in Baolang oil field,

以焉耆盆地宝浪油田宝中区块开发方案设计中建立构造模型的工作为实例,说明在油田开发设计阶段,如何综合利用多种信息,提高构造模型精度。宝中区块整个覆盖三维地震,但地震资料分辨率较低,在完成下侏罗统三工河组3个油组顶面构造图的工作中,首先使用倾角测井资料绘制构造等高线图及构造剖面图,控制工区整体构造形态;结合岩心描述和井间层位对比,了解地层横向变化基本规律及岩性纵向变化以及相应井旁地震道的地震响应;依据勘探阶段完成的构造图,参考据井孔崩落扩径方向确定的现今最大水平主应力方向,恢复古构造并模拟古构造应力场,计算目的层位平面破裂值强度,指示断层和裂缝发育情况;使用均方根振幅剖面解释小断层;完成构造图后,利用平面流体模型、流体分布的重力分异合理性,复查地震解释的断层。根据用该方法完成的最终构造图,部署了3口井,其中宝203井和宝205井实际钻遇的各油组顶面深度与构造图解释深度的误差最大为1.4m,最小为0.4m。图4表3参1(王孝陵摘)

A superimposed basin is mainly characterized by several evolution stages. In different stage, the basin types and characters are different. Taking Tarim and Qaidam basins of China for examples, the basins experienced three open\|close cycles since Sinian. They are Sinian\|Middle Devonian, Late Devonian\|Triassic and Jurassic\|Quaternary cycles. The Sinian\|Middle Devonian basin is intra\|cratonic marine basin. The Late Devonian\|Triassic basin is related to back\|arc extension and compression, and it transformed...

A superimposed basin is mainly characterized by several evolution stages. In different stage, the basin types and characters are different. Taking Tarim and Qaidam basins of China for examples, the basins experienced three open\|close cycles since Sinian. They are Sinian\|Middle Devonian, Late Devonian\|Triassic and Jurassic\|Quaternary cycles. The Sinian\|Middle Devonian basin is intra\|cratonic marine basin. The Late Devonian\|Triassic basin is related to back\|arc extension and compression, and it transformed from marine into continental. The Jurassic\|Quaternary basin is continental and has a bearing upon foreland basin. The evolution of superimposed basin resulted in multi\|source, multi\|phase maturation, multi\|direction migration and multi\|accumulation of oil and gas. The superimposed basins have three main migration\|accumulation models: ①radial migration and annular accumulation model, such as circle\|hero mount accumulation belt of western Qaidam basin, in which the hydrocarbon migration direction is perpendicular to the contour lines of the basin; ②foreland migration\|accumulation model, such as Kuqa depression of northern Tarim basin, in which the hydrocarbon migration is parallel to the compression stress from the mountain belts; and ③cratonic migration\|accumulation model, such as northern uplift of Tarim basin, in which oil and gas migrated and accumulated along the major faults and unconformities.

多期叠合盆地的主要特征是盆地经历了多个演化阶段 ,并且在不同演化阶段中具有不同的盆地类型和性质。对中国西北塔里木和柴达木盆地进行了多期叠合盆地油气运聚研究。这两个盆地自震旦纪以来经历了震旦纪中泥盆世、晚泥盆世三叠纪和侏罗纪第四纪等 3个开合旋回 ,在演化过程中出现由海向陆的转化和拉张 -挤压的交替转化 ,形成了油气来自多源、油气形成多期、油气运移多方向、油气聚集多场所的油气运聚特征。多期叠合盆地有 3种基本油气运聚模式 :①放射状运移、环状聚集模式 ,以柴达木盆地西部环英雄岭构造带为代表 ,油气运移方向垂直于构造等高线的方向 ;②前陆油气运聚模式 ,以塔里木盆地库车坳陷为代表 ,油气运移方向平行于造山带挤压应力方向 ;③古生代海相克拉通盆地油气运聚模式 ,油气沿大型断裂带和区域性不整合面运移和聚集

 
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