Rapid Surface Rupture Mapping from Satellite Data: The 2023 Kahramanmaraş, Turkey (Türkiye), Earthquake Sequence

Nadine G. Reitman, Richard W. Briggs, William D. Barnhart, Alexandra E. Hatem, Jessica A. Thompson Jobe, Christopher B. DuRoss, Ryan D. Gold, John D. Mejstrik, Camille Collett, Rich D. Koehler, Sinan Akçiz
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Abstract

Abstract The 6 February 2023 Kahramanmaraş, Turkey (Türkiye), earthquake sequence produced > 500 km of surface rupture primarily on the left-lateral East Anatolian (~345 km) and Çardak (~175 km) faults. Constraining the length and magnitude of surface displacement on the causative faults is critical for loss estimates, recovery efforts, rapid identification of impacted infrastructure, and fault displacement hazard analysis. To support these efforts, we rapidly mapped the surface rupture from satellite data with support from remote sensing and field teams, and released the results to the public in near-real time. Detailed surface rupture mapping commenced on 7 February and continued as high-resolution (< 1.0 m/pixel) optical images from WorldView satellites (2023 Maxar) became available. We interpreted the initial simplified rupture trace from subpixel offset fields derived from Advanced Land Observation Satellite2 and Sentinel-1A synthetic aperture radar image pairs available on 8 and 10 February, respectively. The mapping was released publicly on 10 February, with frequent updates, and published in final form four months postearthquake (Reitman, Briggs, et al., 2023). This publicly available, rapid mapping helped guide fieldwork and constrained U.S. Geological Survey finite-fault and loss estimate models, as well as stress change estimates and dynamic rupture models.
卫星数据快速地表破裂映射:2023 kahramanmaraku,土耳其(t),地震序列
摘要2023年2月6日土耳其kahramanmaraki (t rkiye)地震序列产生>500公里的地表破裂主要发生在东安纳托利亚断层(~345公里)和Çardak断层(~175公里)的左侧。限制诱发断层上地表位移的长度和大小对于损失估计、恢复工作、快速识别受影响的基础设施和断层位移危害分析至关重要。为了支持这些工作,我们在遥感和现场团队的支持下,从卫星数据中快速绘制了地表破裂图,并向公众发布了近乎实时的结果。2月7日开始进行详细的地表破裂测绘,并继续进行高分辨率(<来自WorldView卫星(2023 Maxar)的1.0 m/pixel光学图像可用。我们分别从2月8日和10日的Advanced Land Observation Satellite2和Sentinel-1A合成孔径雷达图像对获得的亚像素偏移场中解释了最初简化的破裂轨迹。该地图于2月10日公开发布,并经常更新,并在地震后四个月出版最终版本(Reitman, Briggs, et al., 2023)。这种公开的、快速的制图帮助指导了现场工作,并限制了美国地质调查局有限断层和损失估计模型,以及应力变化估计和动态破裂模型。
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