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Coseismic and Postseismic Displacement of 2011 Mw 6.8 Tarlay Earthquake, Myanmar using InSAR Techniques and Inversion Analysis

机译:使用InSAR技术和反演分析的缅甸2011年Mw 6.8 Tarlay地震的震级和震后位移

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In this study, we investigate the March 24th 2011 Mw=6.8 Tarlay earthquake, Myanmar using Interferometric Synthetic Aperture Radar (InSAR) and inversion analysis. We firstly invert InSAR coseismic displacement from our previous study. The inversions are carried out in both single and multi-patch model. The coseismic slip of 2.5 meter from single-patch solution is then combined with long-term slip rate from geomorphological study, resulting in an estimate of 1,140-4,160 years recurrence period. Then, coulomb stress changes on nearby faults in northern Thailand are calculated. It is found that stress in western and middle segments of Mae Chan fault decreases significantly while stress increase in eastern segment of Mae Chan, Mae Ing and Chiang Kham fault. Finally, the results from PSInSAR of 29 Radarsat-2 images reveal postseismic displacement rates between -24.4.6 to 34.5 millimeters per year (51 views)
机译:在这项研究中,我们使用干涉式合成孔径雷达(InSAR)和反演分析调查了2011年3月24日缅甸Mt = 6.8泰雷地震。我们首先根据先前的研究反演InSAR同震位移。在单补丁和多补丁模型中都可以进行反演。然后将单块溶液中2.5米的同震滑移与地貌学研究的长期滑移率相结合,得出了1,140-4,160年的复发期估计。然后,计算出泰国北部附近断层的库仑应力变化。研究发现,湄赞断裂带中西部地区的应力显着降低,而湄赞断裂带,湄英断裂和清康断裂带东部地区的应力增加。最后,PSInSAR的29枚Radarsat-2图像的结果表明,地震后的位移速率为每年-24.4.6到34.5毫米(51次观看)

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