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      形变
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  deformation
    Present-day Crustal Deformation in China and GPS-derived Coordinate Time Series Analysis
    中国大陆现今地壳形变与GPS坐标时间序列分析
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    Some Key Issues Relating to High Precision GPS Positioning and Crustal Deformation Analysis
    高精度GPS定位及地壳形变分析若干问题的研究
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    Characteristics of Crustal Motion and Deformation from GPS Monitoring in the Eastern Qinghai-Tibet Plateau and Adjacent Areas
    基于GPS监测的青藏高原东部及邻区地壳运动形变特征研究
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    A Study of Some Problems Concerning the Analysis of Crustal Deformation Surveys
    地壳形变分析中几个问题的讨论
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    The Statistical Test of Deformation Model
    形变模型的统计检验
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  crustal deformation
    Present-day Crustal Deformation in China and GPS-derived Coordinate Time Series Analysis
    中国大陆现今地壳形变与GPS坐标时间序列分析
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    Some Key Issues Relating to High Precision GPS Positioning and Crustal Deformation Analysis
    高精度GPS定位及地壳形变分析若干问题的研究
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    A Study of Some Problems Concerning the Analysis of Crustal Deformation Surveys
    地壳形变分析中几个问题的讨论
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    ERROR ANALYSIS ON THE KINEMATIC DESCRIPTION OF CRUSTAL DEFORMATION
    地壳形变运动模型的误差分析
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    ESTIMATION OF A LINEAR MODEL WITH NON-STATIONARY NOISE AND ITS APPLICATION TO CRUSTAL DEFORMATION
    一类非平稳噪声线性模型的估计及其在地壳形变中的应用
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  crust deformation
    LEVELING STAFF ERROR AND ITS INFLUENCE ON DATA OF VERTICAL CRUST DEFORMATION
    标尺误差及其对垂直形变资料的影响
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    PRACTICE OF CRUST DEFORMATION MONITORING USING GPS TECHNIQUE
    利用GPS技术监测地壳形变的实践
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    Establishment and Precision Analysis of Crust Deformation GPS Monitoring Networkin Northeastern Margin of the Qinghai-Tibetan Plateau
    青藏高原东北缘地壳形变GPS监测网的建立和精度分析
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    Outline of Digital crust deformation observation network of Fujian province
    “十五”福建省地壳形变数字化监测网简介
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    The Late Pleistocene deposits and paleoenvironments and their bearing on crust deformation in the Shenhu Bay of Fujian Province,China
    福建深沪湾晚更新世沉积、古环境和地壳形变
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  “形变”译为未确定词的双语例句
    Studies on the Models of Vertical Crustal Movements
    地壳垂直形变模型的研究
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    OPTIMIZATION AND DESIGN OF DEFORMING NETWORKS
    形变监测网的设计与优化
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    The Systematical Error Analysis of Baseline Processing in GPS Network
    GPS形变监测网基线处理中系统误差的分析
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    Graphics Update Processing of the Cadastral Spatial Entities Based on Spatial Topology of SICAD/Open
    基于SICAD/Open空间拓扑结构的地籍空间实体图形变更处理
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    Development of the Simulation Techniques of Vertical Crustal Movement of China
    地壳垂直形变场拟合技术在中国的发展
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  deformation
       Our main achievement is that any Schubert variety admits a flat deformation to a union of normal toric varieties.
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       The corresponding monodromyre presentation of the braid group Bg of type g is a deformation of the action of (afinite extension of) W on V.
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       We study a generalization of the isomonodromic deformation to the case of connections with irregular singularities.
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       We call this generalization Isostokes Deformation.
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       A new deformation parameter arises: one can deform the formal normal forms of connections at irregular points.
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  crustal deformation
       The upper-mantle convective flow in the direction of the Indian Plate's motion was the main cause of the crustal deformation.
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       The crustal deformation directions as determined from GPS measurements and seismological observations are found to agree well.
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       Apparently, the crustal deformation due to the sources of the aforementioned earthquakes reaches the central part of the European craton.
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       The main pattern of the crustal deformation is a clockwise rotation vortex structure and a differential slip along the boundary fault between different blocks.
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       Monitoring crustal deformation by GPS and InSAR in the three gorge area
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  crust deformation
       Some earthquakes in recent years (such as Tangshan earthquake (1976, China), North Ridge earthquake (1994, USA), Kobe earthquake (1995, Japan)) did not occur in known faults; moreover, the detailed data of geology, earthquake, crust deformation, etc.
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       Polycrystalline quartz ribbons in high-grade metamorphic rocks from the Daqingshan region, are typical microfabrics of, and provide information for, deep crust deformation and metamorphism.
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       The method of AF synthetic detection on crust deformation anomaly and its application in earthquake prediction
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       In this paper, the unstable model of crust deformation and the anomaly F-detection are discussed.
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       The images of main precursor mode have the characteristic of main shock-after shock type, which is agreement to the model of coupling movement between crust density and crust deformation (DD mode of coupling movement).
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         :
            本文首先推导了空中三角测量系统误差的传播规律。然后利用方格网在精密立体测图仪上进行了一些空中三角测量,并根据相同假定的已知控制点,分别利用了二次、三次多项式,及二次、三次正形变换公式等平差公式进行归算。由观测成果的分析,求出了各外方位元素系统的变形数值,并进行了比较。对上述各种不同平差公式的效果,根据实验分析的结果提出了一些结论。
文摘来源
         This paper presents a new device-a three dimensional reader measuring the fringe shift from the hologram. Measuring data can be obtained with accuracy by free rotation about the measured point of displacement, thereby can be read the angles of various directions of observation and the number of the fringe shift, with the result used as a computer input for obtaining the three cartesian components of displacement. This device is applied to a sphere undergoing radial deformation; the fringe counting results o...
            本文提出一种新的设备——从激光全息图测读条纹标移量的三维读数仪。它能精确地围绕被测形变点自由转动从而读取观察方向变化的角度及相应的条纹飘移故作为计算机的输入而求得形变的三坐际分量。该设备应用于一承受径向变形之圆球壳的分析;十六个变形点的计算结果显示了整个分析表面的径向膨胀量大体相等,并与应变计的测试结果作了比较。研究的结果表明单张全息图的读数仪法能有效地测定各点运动量的大小和方向,预示这种全息条纹分析系统将成为一种很有用的工程工具。
文摘来源
         In this paper, a dynamic adjustment method monitoring the horizontal deformation is suggested by the adjustment of observation equations with condition equations.The problems about the models of moving stations, types and numbers of condition equations, configuration and data defects, the way of calculation and accuracy estimation are discussed. Then a numerical example is given.This method is characterized by effectivelly utilization of all observational data, especially will give the best results for the ...
            本文提出了应用带条件的间接观测平差进行水平形变网的动态平差方法。研究了点位运动的数学模型,起算条件的类型和数量,网的形亏和秩亏现象,计算的方法和成果的精度估算等问题,并给出了具体的算例。 本方法可用于各种类型的水平监测网。特点是能充分地利用所有的观测资料,特别对那些延续时间长,观测断续进行,难以分期平差的网,效果更佳。并且由于引入了突变参数,解决了不连续观测中点位突变造成的困难。
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