块体运动

  • 网络mass movement;mass wasting;Mass wasting, mass movement
块体运动块体运动
  1. 岩石风化作用既是地壳固体物质形态转变的重要途径,也是产生块体运动灾害的必要前提条件,其类型和强度受区域气温及降雨条件的控制;

    It is shown that rock weathering is an important way of transforming solid material in the earth crust , and is a necessary condition for the disaster of block mass movement . Its types and intensities are controlled by regional air temperature and rainfall condition .

  2. 东海陆坡海底块体运动地形分析方法

    Methodology for Morphological Analysis of Submarine Mass Movement in the Continental Slope of the East China Sea

  3. 利用GPS资料反演华北块体运动的负位错模型参数

    Negative Dislocation Model Parameters Inverted from GPS Data in North China

  4. 利用GPS时间序列对块体运动进行空间信息分离

    Research of Spatial Separating Method by GPS Time Series

  5. 利用GPS资料浅析华北地区块体运动及与地震活动的关系

    A Brief Analysis of Relation between Block Motion and Seismicity in the North China with GPS Information

  6. 利用1995和1996年华北地区两期GPS复测资料,计算研究了该区现阶段的构造块体运动。

    Based on two periods of GPS remeasurement data of1995 and1996 in North China , the tectonic block movement of this area in present period is calculated and analyzed .

  7. 结合中国地壳运动观测网络及华北地区网实际观测所得的GPS速度场,对华北地区块体运动和应变模型进行了辨识。

    Lastly , using the GPS velocity field coming from Crustal Movement Observation Network of China ( CMONOC ) and North China GPS network , we have identified the models for crustal movement and strain of blocks in North China .

  8. 依据非连续变形数值分析方法(DDA法)的基本理论,提出利用地壳形变观测资料解算块体运动及其应力场的位移载荷法,给出了相应的计算公式。

    On the basis of the fundamental theory of discontinuous deformation analysis the displacement loading method is advanced to solve block movement and its stress field with the deformation measurement data and the related equation is given .

  9. 交叉断层的交替活动与块体运动的实验研究

    Experimental study on alternate slip of intersecting faults and block movement

  10. 最小二乘配置方法确定中国大陆主要块体运动模型

    The Determination of Chinese Mainland Crustal Movement Model Using Least-squares Collocation

  11. 将块体运动分解为整体旋转与内部变形。

    We resolve blocks motion into entire rotation and its interior deformation .

  12. 现今板块、块体运动定量模型的发展

    Development of quantitative model of current plate and blocks motion

  13. 高速滑坡远程预测的块体运动模型

    Kinematic block model of long run-out prediction for high-speed landslides

  14. 亚洲区域构造块体运动模型的建立及其运动学分析

    The kinematic analysis and construction of the tectonic blocks motion model in Asia

  15. 利用非连续变形数值方法研究块体运动及其应力场初探

    Preliminary study on block movement and its stress field by discontinuous deformation analysis

  16. 推导了块体运动和应变的各种模型,讨论了各种模型的适用条件。

    Models for crustal movement and strain of blocks are derived in this paper .

  17. 大陆岩石圈解耦及块体运动讨论以青藏高原川滇地区为例

    Continental lithosphere decoupling : implication for block movement

  18. 初始应力对应力波传播及块体运动规律影响研究

    Study on effects of initial stress on stress wave propagation and block movement law

  19. 中国大陆西部地区现今的块体运动

    Observation and study with GPS on current block moverment in western region of China Continent

  20. 依据古地磁资料探讨华北和华南块体运动及其对秦岭造山带构造演化的影响

    Evolution of the Qinling fold belt and the movement of the north and South China blocks : the evidence of Geology and Paleomagnetism

  21. 首都圈地区的地震多发生于地壳的中、上部,可能存在局域构造块体运动变形和深部构造动力作用的二种不同地震构造成因;

    The vast majority of the earthquakes are located in the upper and middle crust , which implies the two potential seismotectonic mechanisms with deep dynamics and local tectonic blocks motion and deformation .

  22. 在此基础上,假定滑体的运动形式是连续可变的,建立了预测高速滑坡远程的块体运动模型。

    Then on the assumption that the motion form of high speed landslide is continuous and variable , the kinematic block model of long run out prediction for high speed landslides is presented .

  23. 依据非连续变形正分析方法的基本理论,提出了一种考虑多块体运动系统中特定块体边界允许适量侵入的方法&子矩阵调整法,并给出了相应的调整公式。

    On the basis of the discontinuous deformation positive analysis , the submatrix modulation method is presented to consider the appropriate invading of specific block boundary in many-block motion system , and the corresponding modulation formulas are given .

  24. 这种差异除水动力冲蚀外,另一个重要的原因是浅地层土体块体运动使局部浅水区表层沉积物向深水洼地填充,减缓了深水洼地加深速率。

    Except hydropower wash , another important cause of the difference is that shallow stratum soil mass bulk movement make local shallow surface sediment fill deep water bottomland , so slow up the deep rate of deep water bottomland .

  25. 本文概述了数字人体系统层圈块体运动惯量一次矩和质心,介绍了数字人体系统层圈块体运动惯量的应用;

    The once quadrature and matter center of movement inertia of layer-circle block-body of digital human body system were summarized in this article . The application of movement inertia of layer-circle block-body of digital human body system was introduced .

  26. 分析结果表明,中国海岸构造变形的平面和纵断面图象与海岸构造格局一致:北方海岸大面积升降区比较完整,分界明显,表现出大范围块体运动特征;

    The analyses show that the section and profile maps of China coast tectonic deformation are consistent with the coast tectonic pattern : the northern coast is characterized by large area rise drop zones with obvious boundaries , showing effects of large scale crustal movement ;

  27. 按弧后主动扩张说、弧后被动拉张说、局部区域左行挤出说等,演绎出的盆地空间几何形态与实际情形不符,演绎出的块体运动及位移在空间上不能平衡。

    The basins ' spatial geometric forms deduced from the hypotheses of back arc active extension , back arc passive tension and regional left lateral extrusion do not coincide with the actural ones ; and the deduced block movement and displacement do not balance in space .

  28. 本文主要利用GPS等空间大地测量手段的直接和间接观测资料,对形变分析背景场的定义、性质以及其建立方法进行了研究,并建立了全球主要板块和中国大陆内部块体的运动模型。

    In this paper we study the difinition , characters and establishment of the background field of the crustal deformation , the global plate motion models and Chinese plate motion models based on the direct measurements and indirect ones from space geodesy .

  29. 相对位于东部的稳定点组,东北块体向北运动,位移量约10mm;华南块体向东南运动,位移量约9mm。

    With reference to a group of stable stations with small relative movement in the eastern part of China , the northeastern China block moved northward for about 10 mm , the southeastern China block moved southeastward for about 9 mm .

  30. 爆炸荷载作用下深部块体变形运动规律研究

    Study on rule of Block Deformation and movement under explosion loads