2025/06/11 by Hirano, Shiro, Doke, Ryosuke, Maeda, Takuto
#FOS: Physical sciences #Geophysics (physics.geo-ph)
paper · doi:10.48550/arxiv.2506.09652
We investigated the rupture dynamics of the 2025 Mw7.7 Mandalay, Myanmar earthquake, using a video recording of surface rupture, strong motion recordings, waveform simulation, and satellite imagery. Our assessment, based on the S-wave observation in the video and rupture arrival time at a seismic station 246 km south of the hypocenter, suggests that rupture decelerated to subshear speeds (∼3 km/s) from initial supershear propagation (∼6 km/s) before reaching the camera location. This deceleration is also supported by comparison between the fault-normal acceleration patterns seen in the video and that simulated by kinematic rupture modeling. Additionally, satellite imagery indicated a local minimum in slip (2-3 m) approximately 40-60 km south of the epicenter, suggesting a region of reduced stress drop that likely caused the temporary deceleration. Beyond this point, the rupture appears to have re-established supershear propagation.