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垂向
相关语句
  vertical
    CALCULATION OF HIGHER EVEN VERTICAL DERIVATIVES OF POTENTIAL FIELD BY SPLINE FUNCTION B
    用B样条函数计算位场垂向高偶阶导数
短句来源
    VERTICAL RESOLUTION OF ZERO-PHASE WAVELETS
    零相位子波的垂向分辨率
短句来源
    STUDY OF THE VERTICAL MIGRATION OF THE LIGHT HYDROCARBON OF THE ARLAXING-ERZHAN AREA IN THE SONGLIAO BASIN
    松辽盆地阿拉新—二站地区轻烃垂向迁移规律研究
短句来源
    Chemical types of ooze water in vertical profile and their formation mechanism in the Northern part of South China Sea
    南海北部软泥水化学垂向剖面类型及其形成机制
短句来源
    VERTICAL DIFFERENCE OF WATER QUALITY IN OBSERVATION WELL AND ITS INFLUENE ON SAMPLING
    观测井水质垂向差异及对取样质量的影响
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  vertical direction
    APPLICATION OF FLUORESCENCE SPECTRUM TO STUDIES OF HYDROCARBON MICRO MIGRATION IN VERTICAL DIRECTION
    荧光光谱在烃类垂向微运移研究中的应用
短句来源
    Study of Superimposed Seismic Source in Vertical Direction on High Distinguishability Exploration
    高分辨率地震勘探的垂向叠加震源研究
短句来源
    (2) Surface (0-75m) , hyposurface (75-300m) , intermediate (300-1000m) and deep ( 1000-3000m) water mass can be classified in vertical direction.
    (2)南海垂向上水团分布大概可基本划分为:表层水团(0—75m)、次表层水团(75—300m)、中层水团(300—1000m)和深层水团(1000—3000m)。
短句来源
    Storage capacity (permeability, transmissibility) of massive thickness aquifer will show negative index change ( y=Ax -B ) as the depth row in vertical direction, while it shows power function change ( y=AH ±B ) in the horizontal direction.
    巨厚含水层富 (透、导 )水性随垂向深度呈负指数 (y =Ax-B)变化 ,水平方向上随埋深标高呈幂函数 (y =AH±B)变化 ;
短句来源
    In the vertical direction, the salt water penetrated for 0.5 m ~ 1.67 m downward every year.
    垂向上咸水体年下移速率一般每年0.5~1.67m。
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  “垂向”译为未确定词的双语例句
    CHARACTERISTICS OF THE SPECTRAL CURVES OF THE PERPENDICULAR SUPERPOSED MAGNETIC BODIES
    垂向叠加磁性体谱曲线的特征
短句来源
    MULTIFREQUENCY BACKSCATTERING TOMOGRAPHY IN A VERTICALLY VARYING BACKGROUND
    垂向非均匀背景多频背向散射层析成像
短句来源
    R factor Analysis in Pertroleum Exploration Comprehensive Assessment
    R型因子分析和油气区带评价的多层系垂向叠合
短句来源
    APPLICATION OF VC FOR REALIZING RAY TRACING AND ISOCHRONECONSTRUCTION IN VERTICALLY INHOMOGENEOUS MEDIA
    垂向不均匀介质中射线追踪及等时线构造的VC实现
短句来源
    Geochemical Characteristics of Soil down Profile around Poyang Lake and Determination of Ⅰ Environment Depth
    江西鄱阳湖周边地区土壤垂向剖面地球化学特征及第Ⅰ环境深度的确定
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  vertical
In order to deal with large problems, a pair of trust region subproblems in horizontal and vertical subspaces is used to replace the general full trust region subproblem.
      
The horizontal trust region subproblem in the algorithm is only a general trust region subproblem while the vertical trust region subproblem is defined by a parameter size of the vertical direction subject only to an ellipsoidal constraint.
      
That is, the plot with the fitted response ? on the horizontal axis and the observed y on the vertical axis can be used to visualize the link function.
      
It was found that the vertical magnetic anisotropy would drop lineally with the increase of the array diameter.
      
In contrast, under AFM nanoindentation mode, the tip-induced crystallization occurred when a sufficiently high vertical tip force was applied to the melt droplets of PEO with Mn ? 1.0 × 104 g/mol.
      
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  vertical direction
The horizontal trust region subproblem in the algorithm is only a general trust region subproblem while the vertical trust region subproblem is defined by a parameter size of the vertical direction subject only to an ellipsoidal constraint.
      
This method is different from classical algorithms in which the gray differential values of the mutual vertical direction are combined into one gradient value.
      
The stretching of a liquid sample, squeezed out in the vertical direction from an aperture of an arbitrary form, is investigated.
      
A study is made of the parametric excitation of internal waves in a continuously stratified liquid in a vessel executing oscillations in the vertical direction.
      
In [2, 3] the effect of high-frequency harmonic vibration in the vertical direction on the stability of this flow was investigated.
      
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Sequences of 11 major earthquakes occurred in the continental area of China have been analysed for the characteristics of their spatial distribution of large aftershocks. It is found that:1. The large aftershocks are located in three areas: in the vicinities of the ends of the earthquake fault and the epicenter of the main shock.2. The characteristics of spatial migration of the large aftershocks are as follows: (1) The migration distance of the large aftershocks corresponds to the rupture length of the main...

Sequences of 11 major earthquakes occurred in the continental area of China have been analysed for the characteristics of their spatial distribution of large aftershocks. It is found that:1. The large aftershocks are located in three areas: in the vicinities of the ends of the earthquake fault and the epicenter of the main shock.2. The characteristics of spatial migration of the large aftershocks are as follows: (1) The migration distance of the large aftershocks corresponds to the rupture length of the main shock, and increases with time; (2) The distance and direction of migration are related to the rupture pattern. For stronger main shocks with unilateral rupture, the migration of large aftershocks relative to the epicenter of the main shock will be unilateral; for an earthquake with bilateral rupture, the migration of the large aftershocks will be some what similar to relaxation oscillation from one end of the earthquake fault to the other relative to the epicenter of the main shock. For a twin earthquake (two main shocks), the large aftershocks migrate usually in a unilateral manner relative to the "first main shock" while in a bilateral manner relative to the "second main shock".3. The vertical distribution of the large aftershocks in a section is within the fault plane and mostly are located on the front of the fault.A preliminary theoretical explanation for the above observational results has been attempted based upon the principles of rheology and fracture mechanics.

本文是《强余震的时间分布特征及其理论解释》(地球物理学报,1979年1期)的继续。文中分析了我国11个强震的余震序列,结果表明,强余震的空间分布有以下特点: 1.强余震的平面分布。强余震主要分布在断层的两端附近及主震震中附近。 2.强余震的空间迁移具有以下特征: (1)强余震的迁移范围与主震破裂长度相当,且随着时间的推移,迁移的范围越来越大;(2)其总的迁移范围及迁移方向与主震破裂方式有关。对单侧破裂的较大主震,强余震相对其震中呈单侧迁移;对双侧破裂的主震,其强余震相对其主震震中会呈现松弛振荡式迁移;对于双震型地震,强余震往往对第一个“主震”表现为单侧迁移,对于第二个“主震”表现为两头跳现象。 3.强余震的垂向分布:位于主破裂的断层面内,且在其前缘上。 本文从断裂力学和流变学角度,对上述观测事实进行了初步理论解释。

Taking into account of the three factors of kerogen types(T), temperature

本文提出的定量评价生油岩的TTT法,同时考虑了生油母质类型(T)、有机质成熟的温度(T)和时间(T)三个因素;它采用生油岩中不同类型干酪根在不同热演化阶片上的裂解烃产率、有机碳、氯仿沥青A和总烃等四个参数,可以直接计算生油岩的生烃量和排烃量.本文结合松辽盆地的实际资料,对青一段生油岩的生烃量、排烃量进行了计算,其结果与烃类垂向分布及有机质成熟史相吻合.

After dealing briefly with the development of the concept of meta llotectonies, the paper discusses preliminarily deep-seated structure, tectonic-geochemistry of metallotectonics, and application of the symme tric theory to metallotectonics. The author consider:A) The study of deep-seated structure(geophysic field)is one of the basic contents of metallotectonics. Through study of geophysic features, we can get data on the structure of the crust, the features of vertical or lateral variation of every layer, undulate...

After dealing briefly with the development of the concept of meta llotectonies, the paper discusses preliminarily deep-seated structure, tectonic-geochemistry of metallotectonics, and application of the symme tric theory to metallotectonics. The author consider:A) The study of deep-seated structure(geophysic field)is one of the basic contents of metallotectonics. Through study of geophysic features, we can get data on the structure of the crust, the features of vertical or lateral variation of every layer, undulate variation of Moho disconti nuity, structural variation of areas between continental crust and oce anic crust, etc. On the basis of the data, metallogenic regularities are analysed, and mineral deposits are prognosticated. B) The study of tectonic-geochemistry is a key to metallotectonics. The formation of ore-forming elements geochemical anomalies is not only closely related tp the fractional development stages and produc tions of tectonic-geochemistry of the crust but also controlled by de velopment features which they were undergone after their formation.C) In the last years, application of the symmetric theory to metallo tectonics is further progessive. Many scientists of our country and other countries have applied the theory to metallotectonics of different scales and types, and have achieved some successes in metallogenic progno stication and prospecting. The equidistances of metallogenic structures may be divided into three types: concentric equidistance, en echelon equidistance, parallel equidistance. Their formation mechanism may be related to spreading manner of stress wave.

本文在简述成矿构造概念的演进之后,对成矿构造理论中的深部构造、构造-地球化学的研究及对称理论在成矿构造中的应用等问题,进行了初步研究。作者认为: 1.深部构造(地球物理场)的研究是成矿构造理论研究的一项基本内容。目前主要通过地球物理特征的研究,籍以提供地壳结构,各壳层的垂向或横向变化特征,深部莫氏面的起伏变化,犬陆壳与大洋壳相邻部位的结构变化等方面资料,在此基础上,进行成矿规律分析和矿产预测。 2.构造-地球化学的研究是成矿构造理论研究中的一个关键问题。成矿元素地球化学异常场的形成,与地壳构造、地球化学分异演化阶段和产物的成因紧密相关。同时,又受地球化学异常场形成后其所经历的发展特征所控制。 3.对称理论在成矿构造研究中,近年来有进一步发展。国内、外的学者,把对称理论应用于大、中、小不同类型的成矿构造,在成矿预测、找矿勘探中取得了比较好的效果。对成矿构造的等距性初步可划分为:同心等距、斜列等距、平行等距三种不同类型。其形成机理可能与应力波的传播方式有关。

 
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