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   horizontal deformation field 的翻译结果: 查询用时:0.008秒
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horizontal deformation field
相关语句
  水平形变场
     A DESCRIPTION AND REALIZATION OF HORIZONTAL DEFORMATION FIELD BY THE MULTI-KERNEL FUNCTION
     水平形变场的函数描述及其实现方法
短句来源
     Based on the GPS data of the North China and its adjacent areas surveyed in the past more than ten years and the elastic motion model of Eurasia plate, the horizontal deformation field and local horizontal deformation field in the North China area are obtained. The horizontal deformation field in the North China exhibits a rather consistent movement along the SE while the motion direction turns gradually with clockwise, and the movement rate raises from west to east.
     用华北及邻区近十多年GPS测量结果和欧亚板块的弹性运动模型研究华北地区的水平形变场和局部水平形变场 ,发现华北地区水平形变场存在比较一致的SE向运动 ,且运动方向绕顺时针方向逐渐旋转 ,从西向东运动速率逐渐增大。
短句来源
     Besides the deformation rate for local deformation field in the North China is about 50% of that of the horizontal deformation field. The local deformation directions of Ordos, North China plain and eastern Shandong-Huanghai blocks are SE, SSE and SSW, respectively.
     鄂尔多斯、华北平原和鲁东 黄海地块的局部形变方向分别为SE方向、SSE方向和SSW方向 ,而华北局部形变场的形变速率大约为水平形变场的 5 0 %。
短句来源
     It is inferred on the basis of general characteristics of horizontal deformation field and strain field in the whole area that the main driving forces of the tectonic movement and deformation in the North China are: the NE directional pushing force from Qinghai Tibit plateau, the west directional pushing force to the crust of the North China coming from the underthrust Pacific plate to Eurasia plate, and the NW SE directional extension caused by the uplifting crust.
     根据全区水平形变场与应变场的基本特征推测 ,华北地区构造运动与形变的主要驱动力为 :青藏高原NE方向的推挤力 ,太平洋板块向欧亚板块俯冲对华北地壳产生的西向推挤力 ,以及地壳上隆所产生的NW SE方向的扩张力
短句来源
     In different sections of the Shanxi fault subsidence zone there are differences and temporal variation of horizontal deformation field and strain field calculated from GPS observations.
     根据GPS点观测结果计算得出山西断陷带各地段 1999~ 2 0 0 3年的水平形变场存在差别 ,并有瞬时变化 ,应变场也有同样的情况。
短句来源
  “horizontal deformation field”译为未确定词的双语例句
     HORIZONTAL DEFORMATION FIELD IN HUAILAI- YANQING AREA
     怀来、延庆地区的水平形变
短句来源
  相似匹配句对
     SLAB DEFORMATION IN VERTICAL AND HORIZONTAL PASSES
     板坯在立轧、平轧道次中的变形研究
短句来源
     HORIZONTAL DEFORMATION ANALYSIS FOR WANJIAZHAI DAM
     万家寨大坝水平变形分析
短句来源
     HORIZONTAL DEFORMATION FIELD IN HUAILAI- YANQING AREA
     怀来、延庆地区的水平形变
短句来源
     ON DEFORMATION OF ARCHITECTURE
     论建筑的变形
短句来源
     DEFORMATION AND SUPERCONDUCTIVE
     变形与超导
短句来源
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  horizontal deformation field
This paper improves Bannon's work on the quasi-geostrophic frontogenesis in a horizontal deformation field.
      


Based on the GPS data of the North China and its adjacent areas surveyed in the past more than ten years and the elastic motion model of Eurasia plate, the horizontal deformation field and local horizontal deformation field in the North China area are obtained. The horizontal deformation field in the North China exhibits a rather consistent movement along the SE while the motion direction turns gradually with clockwise, and the movement rate raises from west to east.The motion rates of Ordos,...

Based on the GPS data of the North China and its adjacent areas surveyed in the past more than ten years and the elastic motion model of Eurasia plate, the horizontal deformation field and local horizontal deformation field in the North China area are obtained. The horizontal deformation field in the North China exhibits a rather consistent movement along the SE while the motion direction turns gradually with clockwise, and the movement rate raises from west to east.The motion rates of Ordos, North China plain and Eastern Shandong Huanghai blocks are 4.8 mm/a, 5.0 mm/a and 5.2 mm/a and their motion directions are SE50°, SE40° and SE35°respectively. Besides the deformation rate for local deformation field in the North China is about 50% of that of the horizontal deformation field.The local deformation directions of Ordos, North China plain and eastern Shandong-Huanghai blocks are SE, SSE and SSW, respectively. The relative motion on both sides of major fault zones and the principal strain field in each block are calculated by use of the model with rotation of entire block and linear strain. Basically, the EW and NWW trending faults in the North China are left lateral strike slip ones and the slip rates decrease from east to west,while the NNE and NE trending faults in the North China are right lateral strike slip ones and the slip rates decrease from north to south. The basic frame of strain field in the North China is that: the compression is NEE SWW directional and the extension NNW SSE directional and the principal compressive strain rate increases gradually from west to east and the principal tensile strain rate decreases gradually from west to east. It is inferred on the basis of general characteristics of horizontal deformation field and strain field in the whole area that the main driving forces of the tectonic movement and deformation in the North China are: the NE directional pushing force from Qinghai Tibit plateau, the west directional pushing force to the crust of the North China coming from the underthrust Pacific plate to Eurasia plate, and the NW SE directional extension caused by the uplifting crust.

用华北及邻区近十多年GPS测量结果和欧亚板块的弹性运动模型研究华北地区的水平形变场和局部水平形变场 ,发现华北地区水平形变场存在比较一致的SE向运动 ,且运动方向绕顺时针方向逐渐旋转 ,从西向东运动速率逐渐增大。鄂尔多斯、华北平原和鲁东 黄海地块的运动速率分别为 4 .8mm/a、5 .0mm/a、5 .2mm/a ,运动方向分别为SE5 0°、4 0°、35°。鄂尔多斯、华北平原和鲁东 黄海地块的局部形变方向分别为SE方向、SSE方向和SSW方向 ,而华北局部形变场的形变速率大约为水平形变场的 5 0 %。应用地块的整体旋转与线性应变模型计算了华北主要断裂带两侧的相对运动和各地块内部的主应变场。华北EW向和NWW向断裂基本上为左旋走滑型 ,滑动速率从东向西逐渐减小 ;NNE向和NE向断裂基本上为右旋走滑型 ,从北向南滑动速率逐渐减小。华北地区应变场的基本格架是NEE SWW方向压缩与NNW SSE方向扩张 ,主压应变率从西向东逐渐增大而主张应变率从西向东逐渐减小。根据全区水平形变场与应变场的基本特征推测 ,华北地区构造运动与形变的主要驱动力为 :青藏高原NE方向的推挤力 ,太平洋板块向欧亚板块俯冲对华北...

用华北及邻区近十多年GPS测量结果和欧亚板块的弹性运动模型研究华北地区的水平形变场和局部水平形变场 ,发现华北地区水平形变场存在比较一致的SE向运动 ,且运动方向绕顺时针方向逐渐旋转 ,从西向东运动速率逐渐增大。鄂尔多斯、华北平原和鲁东 黄海地块的运动速率分别为 4 .8mm/a、5 .0mm/a、5 .2mm/a ,运动方向分别为SE5 0°、4 0°、35°。鄂尔多斯、华北平原和鲁东 黄海地块的局部形变方向分别为SE方向、SSE方向和SSW方向 ,而华北局部形变场的形变速率大约为水平形变场的 5 0 %。应用地块的整体旋转与线性应变模型计算了华北主要断裂带两侧的相对运动和各地块内部的主应变场。华北EW向和NWW向断裂基本上为左旋走滑型 ,滑动速率从东向西逐渐减小 ;NNE向和NE向断裂基本上为右旋走滑型 ,从北向南滑动速率逐渐减小。华北地区应变场的基本格架是NEE SWW方向压缩与NNW SSE方向扩张 ,主压应变率从西向东逐渐增大而主张应变率从西向东逐渐减小。根据全区水平形变场与应变场的基本特征推测 ,华北地区构造运动与形变的主要驱动力为 :青藏高原NE方向的推挤力 ,太平洋板块向欧亚板块俯冲对华北地壳产生的西向推挤力 ,以及地壳上隆所产生的NW SE方向的扩张力

In different sections of the Shanxi fault subsidence zone there are differences and temporal variation of horizontal deformation field and strain field calculated from GPS observations.In Shanxi fault subsidence zone,the earthquakes of %M%≥4 occured in the areas where the displacement rate vectors of GPS sites are larger and the larger the magnitudes of earthquakes are, the more distinct the ground deformation features are.In addition the minimal principal strain rate and maximal shear strain...

In different sections of the Shanxi fault subsidence zone there are differences and temporal variation of horizontal deformation field and strain field calculated from GPS observations.In Shanxi fault subsidence zone,the earthquakes of %M%≥4 occured in the areas where the displacement rate vectors of GPS sites are larger and the larger the magnitudes of earthquakes are, the more distinct the ground deformation features are.In addition the minimal principal strain rate and maximal shear strain rate in seismic region is comparatively larger .In the Shanxi fault subsidence zone the differences of the dominant directions of the minimal principal strain axis are obvious in different periods.The angle between the dominant strike of Shanxi fault subsidence zone and the minimal principal strain rate axis is small,and that with the maximal principal strain rate axis is large.Under the joint action of the principal compressive stress and principal tensile stress represented by the minimal and maximal principal strain rate axes,the right-lateral dominant tenso-shear activity ought to take place in Shanxi fault subsidence zone.

根据GPS点观测结果计算得出山西断陷带各地段 1999~ 2 0 0 3年的水平形变场存在差别 ,并有瞬时变化 ,应变场也有同样的情况。山西断陷带内的M≥ 4地震多发生在GPS点位移速率矢量较大的地区 ,且随着震级增大形变特征也愈显著。地震区的最小主应变速率和最大剪应变速率一般都较大 ;最小主应变轴的优势方向各时间段差别较大。山西断陷带的主体走向与最小主应变速率轴夹角较小 ,与最大主应变速率轴夹角相对较大 ,在最小和最大主应变速率轴代表的主压应力和主张应力共同作用下 ,山西断陷带的主体应变发生右旋张剪活动。

 
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