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等温面
相关语句
  isothermal surface
    SOME PROBLEMS ABOUT INTERPRETATION OF LITHOSPHERIC CURIE ISOTHERMAL SURFACE
    岩石圈居里等温面解释的若干问题
短句来源
    Using 3-D magnetosphere inverse theory and method, we process the aeromagnetic data: of Yanqing and Huailai areas, and obtain the buried depth map of Curie isothermal surface and the distribution map of apparent specific magnetizing moment of these areas.
    应用三维磁性层反演理论和方法,对延庆、怀来地区航磁资料进行了数据处理,反演计算了该区磁性基底埋深、居里等温面埋深和视磁化强度分布。
短句来源
    This paper introduces some methods which are applicated to calculate Curie isothermal surface by regional magnetic date.
    介绍了利用区域磁测资料计算居里等温面的几种常用方法。
短句来源
  “等温面”译为未确定词的双语例句
    A CRUSTAL MAGNETIZATION MODEL AND CURIE ISOTHEM
    地壳磁化强度模型和居里等温面
短句来源
    Methods of mapping the depth to the Curie isotherm
    居里等温面深度的探测方法(英文)
短句来源
    Gravimetric data can be used to calculate the thicknesses of sedi-mentary formations, aeromagnetic data may be used to obtain Curie isothermal sur-face,and ground temperature gradient can be thus computed by using Curie-Weiss law.
    利用重力资料可反演出各类沉积岩的厚度,利用航磁资料可反演出居里等温面,再由居里—外斯定律算出地温梯度。
短句来源
    The paper makes theoretical analysis about some important factors, such as selection of regional anomaly and selection of dimension of move windows.
    对影响居里等温面的几个重要因素,诸如区域异常的选择、滑动窗口的尺度选择等进行了理论分析。
短句来源
    According to variable factors effecting temperature of lithologic Curie point, a method used to assent accuracy of Curie surface is given.
    根据影响岩石居里点温度的各种因素,提出评估居里等温面计算精度的方法。
短句来源
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  isothermal surface
The flow past a circular cylinder with an isothermal surface at Mach numbers M∞=2 and 5 and Reynolds numbers ranging from 104 to 108 is investigated on the basis of the Reynolds equations using a differential two-equation turbulence model.
      
Supersonic Flow Past a Circular Cylinder with an Isothermal Surface
      
Supersonic perfect-gas flow past a circular cylinder with an isothermal surface is investigated at the Mach number 5 and Reynolds numbers ranging from 30 to 500,000.
      
Results are given of numerical simulation of hydrodynamics and heat transfer under conditions of transverse flow past a two-dimensional "trench" (a groove whose cross section has the form of a segment of circle) located on a plane isothermal surface.
      
Results are given of numerical simulation of hydrodynamics and heat transfer under conditions of transverse flow past a two-dimensional "trench" (a groove whose cross section has the form of a segment of circle) located on a plane isothermal surface.
      
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Using 3-D magnetosphere inverse theory and method, we process the aeromagnetic data: of Yanqing and Huailai areas, and obtain the buried depth map of Curie isothermal surface and the distribution map of apparent specific magnetizing moment of these areas. The quantitative characteristics of the magnetic basement of the four correlative basins-Yanqing, Fanshan, Huailai and Zhuolu-are revealed. Investigation is conducted into the deep cause for earthquake occurrence and into the relation between crustal blocks...

Using 3-D magnetosphere inverse theory and method, we process the aeromagnetic data: of Yanqing and Huailai areas, and obtain the buried depth map of Curie isothermal surface and the distribution map of apparent specific magnetizing moment of these areas. The quantitative characteristics of the magnetic basement of the four correlative basins-Yanqing, Fanshan, Huailai and Zhuolu-are revealed. Investigation is conducted into the deep cause for earthquake occurrence and into the relation between crustal blocks with different physical nature and seismicity in these areas. Characteristics, of earthquake distribution in these areas is also studied. Earthquake risk zoning and major zones for future monitoring in these areas are preliminarily POinted out.

应用三维磁性层反演理论和方法,对延庆、怀来地区航磁资料进行了数据处理,反演计算了该区磁性基底埋深、居里等温面埋深和视磁化强度分布。揭示了延庆盆地、矾山盆地、怀来盆地、涿鹿盆地等四个相互联通盆地的磁性基底的定量特征。对该区地震发生的深部原因和地壳内不同物性块体与地震的关系进行了探讨;对该区地震分布的特点进行了研究;初步提出了该区地震的危险区划和今后的重点监测区。

There are two important parameters for evaluating hydrocarbon resources in a sedimentary basin, namely, the proportion of source rock and the temperature at which organic substance in source rock changes into hydrocarbon. The former origi-nates hydrocarbon,and the latter controls hydrocarbon generation level and the con-sequent variation. Gravimetric data can be used to calculate the thicknesses of sedi-mentary formations, aeromagnetic data may be used to obtain Curie isothermal sur-face,and ground temperature...

There are two important parameters for evaluating hydrocarbon resources in a sedimentary basin, namely, the proportion of source rock and the temperature at which organic substance in source rock changes into hydrocarbon. The former origi-nates hydrocarbon,and the latter controls hydrocarbon generation level and the con-sequent variation. Gravimetric data can be used to calculate the thicknesses of sedi-mentary formations, aeromagnetic data may be used to obtain Curie isothermal sur-face,and ground temperature gradient can be thus computed by using Curie-Weiss law. As a result,people can estimate source rock volume within the threshoId temper-ature of hydrocarbon generation,then predict hydrocarbon resources.

评估沉积凹陷的含油气性有两个重要参数,即生油岩所沉积的比例和生油岩中有机质向油气的转化温度。前者控制油气资源的生成;后者控制油气的生成及其以后的变化。利用重力资料可反演出各类沉积岩的厚度,利用航磁资料可反演出居里等温面,再由居里—外斯定律算出地温梯度。据此,即可算出生油门限温度范围内的沉积岩中生油岩的体积,预测油气资源量。

In this paper,the authors use 3-D magnetic stratum inversion calculation to study the relief of Curie iso-geothermal surface in Bohai Sea and its abjacent regions,and along with the surface heat flow,the electrical structure of crust and upper mantle,analyze the deep seated geological characteristics.It is found that in Bohai Sea and the region from Kenli to Huanghekou in the northern part of Qiyang depression,the depths of Curie surface is only 13~20km while it reaches 22~24km at Jiao-Liao and Chengde region.The...

In this paper,the authors use 3-D magnetic stratum inversion calculation to study the relief of Curie iso-geothermal surface in Bohai Sea and its abjacent regions,and along with the surface heat flow,the electrical structure of crust and upper mantle,analyze the deep seated geological characteristics.It is found that in Bohai Sea and the region from Kenli to Huanghekou in the northern part of Qiyang depression,the depths of Curie surface is only 13~20km while it reaches 22~24km at Jiao-Liao and Chengde region.The aim of our research is to Present new suggestions for the earthquake zoning and the earthquake disaster prevention.

采用三维磁性层反演方法,研究了渤海及周边地区的居里等温面起伏。结合地表热流值、地壳厚度及地壳上地幔的电性结构,分析了研究区的深部地质特征。发现渤海及济阳坳陷北部的垦利至黄河口地区,居里面的深度只有13~20km,而胶辽和承德地区却深达22~24km。该项研究旨在对地震区划的深部构造背景问题提出新的建议。

 
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