首页> 外文期刊>Geomatics,Natural Hazards & Risk >Active interseismic shallow deformation of the Pingting terraces (Longitudinal Valley ?¢???? Eastern Taiwan) from UAV high-resolution topographic data combined with InSAR time series
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Active interseismic shallow deformation of the Pingting terraces (Longitudinal Valley ?¢???? Eastern Taiwan) from UAV high-resolution topographic data combined with InSAR time series

机译:结合InSAR时间序列的无人机高分辨率地形数据对平亭阶地(台湾东部纵谷)的主动地震活动浅层变形

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ABSTRACT We focus herein on the location, characterization and the quantification of the most active structural feature of Taiwan: the Longitudinal Valley Fault that corresponds to the suture in between the Philippine and Eurasian Plates. In order to determine and monitor its present inter-seismic deformation, we focus on the Pingting Terraces area, situated in the South Longitudinal Valley (Eastern Taiwan). We first determine the structural geometry issued from both photo-interpretation deduced from new unmanned aerial vehicle (UAV) high-resolution Digital Terrain Model data that we acquired (34.78 km 2 with 7.73 cm ground sampling distance), combined with geological field work. In order to characterize and quantify the present deformational patterns over the Pingting terraces, we used an InSAR time series Interferometry algorithm (MT-InSAR) applied to nine L-band SAR images from ALOS satellite acquired over the period 2007?¢????2010. The unprecedented density of measurements (about 120 points per km 2 for a total of 6,400 points) gives a continuous overview of the inter-seismic shallow deformation. The structural geometry combined with the mean velocity map (MT-InSAR) reveals two clear active faults situated above the scarps of the Pingting terraces and responsible for up to 7 and 20 mm/yr velocity offset????along the radar line of sight. A temporal analysis of the deformation is performed with one measurement at each SAR acquisition date, giving major improvements in the characterization and quantification of the Longitudinal Valley active Fault trace.
机译:摘要我们在此集中讨论台湾最活跃的结构特征:与菲律宾板块和欧亚板块之间的缝合线相对应的纵谷断层的位置,特征和定量。为了确定和监视其当前的地震间形变,我们重点研究位于南纵谷(台湾东部)的坪台地区。我们首先确定从我们获取的新无人机(UAV)高分辨率数字地形模型数据得出的照片解释得出的结构几何形状(34.78 km 2,地面采样距离为7.73 cm),再结合地质野外工作。为了表征和量化平顶阶地上的当前变形模式,我们将InSAR时间序列干涉测量算法(MT-InSAR)应用于从ALOS卫星获取的9个L波段SAR图像,该图像是在2007年期间获取的。 2010。前所未有的测量密度(每km 2约有120个点,总共6400个点)连续不断地概述了地震之间的浅层变形。结构几何形状与平均速度图(MT-InSAR)相结合,揭示出位于坪顶阶地陡坡上方的两个清晰的活动断层,可引起高达7和20毫米/年的速度偏移-沿着雷达视线。在每个SAR采集日期对变形进行时间分析,从而进行了一次测量,从而大大改善了纵谷活动断层迹线的表征和定量。

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