基于InSAR的花莲形变监测分析OA
InSAR-Based Monitoring and Analysis of Vertical Deformation in Hualien
以2024年4月3日花莲MS7.3地震前后的地表垂直形变为研究对象,基于覆盖地震事件前后共20景的Sentinel-1A SAR影像,利用PS-InSAR技术获取了花莲及周边地区长时间序列的垂直形变场.通过结合台湾东部地质构造背景,分析了不同地貌和构造单元的形变特征,结果表明:时序InSAR技术能够有效克服气象和地域限制,实现地震频发地区的大范围、长周期形变监测,其中城市区域因干涉相干性更高,监测结果优于森林覆盖区域;位于河流相沉积物带的区域(如花莲县城及溪流下游)在地震后产生较强烈的震后效应,而森林覆盖的构造带则未观测到显著的震后形变信号;此次地震引发的显著形变区域呈现近NE-SW走向的规则椭圆形空间分布,其长轴方向与花东纵谷断裂带走向一致,且地震引起的形变强度由沿海向内陆呈现递减特征.
This study focuses on the vertical surface deformation before and after the MS7.3 Hualien earthquake on April 3,2024.Based on a total of 20 Sentinel-1A SAR images covering the pre-and post-earthquake events,the paper obtained the long-time series vertical deformation field of Hualien and its surrounding areas using PS-InSAR technology.By integrating the geological and tectonic background of eastern Taiwan,the paper analyzed the defor-mation characteristics of different geomorphic and tectonic units.The results indicate that time-series InSAR tech-nology can effectively overcome meteorological and geographical constraints and achieve large-scale,long-term monitoring of surface changes in earthquake-prone areas.Among these areas,urban regions have better monitoring results than forested areas due to higher interferometric coherence.Areas underlain by fluvial sedimentary deposits(such as Hualien County and the lower reaches of streams)exhibit significant post-seismic effects,whereas no clear post-earthquake surface change signals were found in forest-covered geological zones.The area with obvious surface changes caused by this earthquake is shaped like a regular ellipse,extending nearly in the NE-SW direc-tion.The long axis is consistent with the strike of the Hualien-Taitung Longitudinal Valley Fault Zone,and the de-formation intensity caused by the earthquake decreases from the coast toward the inland.
关玉梅;洪旭瑜;胡礼珍;秦双龙
福建省地震局,福州 350003福建省地震局,福州 350003厦门大学 海洋与地球学院,厦门 361102福建省地震局,福州 350003
天文与地球科学
花莲MS7.3地震PS-InSAR形变速率垂直形变
Hualien MS7.3 earthquakePS-InSARDeformation rateVertical deformation
《华南地震》 2026 (3)
23-29,7
福建省地震局科技基金面上项目(M202503)中国地震科技星火计划项目(XH231305YA)厦门市自然科学基金项目(3502Z202573006)联合资助.
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