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   构造等高线图 的翻译结果: 查询用时:0.028秒
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构造等高线图
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  相似匹配句对
     “L-STRUCTURE”FOR FUZZY SET IN A LINEAR SPACE
     L—构造
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     The X.
     在构造 X.
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     Structural Analysis of Coal-Floor Contour Map
     煤层底板等高线上的构造分析
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
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     CONSTRUCTION OF 114—CUBIC GRAPHS
     114—三次构造
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  structure contour map
Several extensive `Hinge faults' that abut at high angles to the arc orientation, are inferred from aninterpretation of the structure contour map.
      
Structure contour map of top salt or equivalent salt weld in Northern Green Canyon.
      
  structural contour map
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.
      
Structural contour map of the top of Miocene basalt basement rocks, Western Snake River Plain, Idaho.
      


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)

In order to picture the evolution of 3 D structure in a basin, it was necessary to compile a series of paleo structural contour maps in varied epochs. The project of compiling paleo structural contour map was a complex research process, in which the researchers might meet various conceptual and technical problems, and whole the process should be restricted by concept of "balance in geology". This paper discussed some key problems, such as how to select a logical model of deformation, how to restore the...

In order to picture the evolution of 3 D structure in a basin, it was necessary to compile a series of paleo structural contour maps in varied epochs. The project of compiling paleo structural contour map was a complex research process, in which the researchers might meet various conceptual and technical problems, and whole the process should be restricted by concept of "balance in geology". This paper discussed some key problems, such as how to select a logical model of deformation, how to restore the denuded thickness and distribution, how to restore displacement of faults, how to do de compaction correction and so on. An acceptable method should be as follows: an upper structure contour map representing a definite geological epoch being restored to horizontal first, then to restore the geometry of the structural contour maps below the upper structure contour map according to geological epoch under restriction of "balance in geology". To compile a reasonable paleo structural contour map, it was necessary to have not only a series of high quality structural contour maps but also some important assistant maps and data, for example, profile sections of tectonic evolution, isopach map of erosion, table of de compaction correction and so on. The paleo structural contour map restored by concept of "balance in geology" might be more reasonable to depict the 3 D structural geometry in the geological epochs than the map compiled by utilizing the thickness of relict strata.

为了描述盆地三维构造的演化过程 ,通常需要编制不同地质时期的古构造等构造线图。编制古构造等高线图是一个复杂的研究过程 ,可能遇到许多概念性和技术性问题 ,但是所有问题都必须在“地质平衡”概念约束下寻求解决途径。本文讨论了按照地质平衡概念编制古构造等高线图的基本原则和可能的技术方案 ,包括研究构造变形模式、复原剥失厚度及其分布、复原断层位移、去压实校正等。运用“地质平衡”概念将较浅地层界面的构造等高线图复原到代表特定地质时期地形面的原始状态 ,相应地将较深地层界面的构造等高线图复原得到的古构造等高线图。运用“地质平衡”概念编制的古构造等高线图比传统的只用地层残余厚度编制的古构造等高线图能更合理地反映地质时期的盆地古构造三维几何特征。

 
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