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Integrated C and L-band Satellite Interferometry for Investigation of Surface Deformation in Northern Vietnam fault zone

机译:集成的C和L波段卫星干涉测量技术,用于调查越南北部断裂带的表面变形

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In this research, we employed satellite Differential Interferometric Synthetic Aperture Radar (DInSAR) in the area of interest to observe the surface deformation at high spatial density. DInSAR has proven to have potential capability to sub-centimeter in scale, thus it is well suited to observe deformation at depth of the inter-plate thrust motion along the major fault of this area, but also offer an opportunity to observe the seismic deformation at the inter-plate shallow thrust fault zone. In this study, we used images acquired from C-band data of ENVISAT and L-band data of ALOS/PALSAR on the experimental area so as to make the dual band interference procedure. It was helpful to continue to make observation as well as analysis. This study also produced the artificial ground control points using C-band time-delayed satellite active radar calibrator to carry out the precise mergence. Finally, it was considered that the materials which made the analysis would contrast with the other materials further. Based on the preliminary study results to show that the tectonic activities had the difference between the northern and southern sections of the Ailao-Red River sheared zone(A-RRSZ) in 1996~2004. Besides, its amount of variation had approximately 6-10 centimeters every year in the northern section. Second, on account of mountainous regions and plateaus, tropical monsoon climate, high temperature and numerous rainfall in northern Vietnam, it was observed the distribution of alluvia flushed around Red River delta, as well as the situation of local resident artificial activity to influence the surface change nearby Hanoi. Further, the change quantity was also estimated.
机译:在这项研究中,我们在目标区域采用了卫星差分干涉合成孔径雷达(DInSAR)来观察高空间密度下的表面变形。事实证明,DInSAR具有潜在的扩展能力,可在亚厘米范围内观测,因此非常适合观察沿该区域主要断层的板间推力运动深度处的形变,但也提供了观察下层地震变形的机会。板间浅冲断层带。在这项研究中,我们使用在实验区域上从ENVISAT的C波段数据和ALOS / PALSAR的L波段数据获取的图像,以进行双波段干扰程序。继续进行观察和分析是有帮助的。这项研究还使用C波段时延卫星有源雷达校准器产生了人工地面控制点,以进行精确的合并。最后,认为进行分析的材料将与其他材料进一步形成对比。初步研究结果表明,1996〜2004年哀牢山-红河剪切带南北段的构造活动有所不同。此外,北部地区每年的变化量约为6-10厘米。其次,由于山区和高原,热带季风气候,高温和越南北部的大量降雨,观察到红河三角洲周围冲积的Alluvia分布以及当地居民影响地表的人工活动的情况换河内附近。此外,还估计了变化量。

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