- 1Université de Toulouse, CNRS, Observatoire Midi-Pyrénées, IRAP, Toulouse, France. (soumaya.latour@irap.omp.eu)
- 2Navier, ENPC, Institut Polytechnique de Paris, Université Gustave Eiffel, CNRS, Marne-la-Vallée, France.
- 3Laboratoire de Géologie, École Normale Supérieure, CNRS, UMR 8538, PSL Université, Paris, France.
- 4Université Côte d’Azur, CNRS, Observatoire de la Côte d’Azur, IRD, Géoazur, Sophia Antipolis, France.
- 5Southern California Edison, Rosemead, CA, USA.
We present the analysis of the first known video of co-seismic slip on a natural fault. It was captured during the 2025 Mw 7.7 Mandalay earthquake (Myanmar) by a CCTV camera located a few meters away from the fault. By direct image analysis of the footage, we measure the slip and slip-rate functions from the natural coseismic rupture. The results show that the rupture propagated as a slip-pulse, with a local slip duration of 1.4 s and a maximum slip rate of 3.5 m/s ± 20%. We then fit two steady-state slip-pulse models to the measured slip-rate function, allowing us to estimate the mechanical properties of the fault: the slip-stress curve, the slip-weakening distance, the breakdown work and the energy release rate. This study shows the value of direct on-fault slip measurements for constraining those mechanical parameters, that are key inputs in dynamic rupture models.
How to cite: Latour, S., Lebihain, M., Bhat, H. S., Twardzik, C., Bletery, Q., Hudnut, K. W., and Passelègue, F.: Direct estimation of earthquake source properties from a single CCTVcamera (2025 Mw 7.7 Mandalay earthquake, Myanmar), EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-21737, https://doi.org/10.5194/egusphere-egu26-21737, 2026.