Extended Data Fig. 5: Teleseismic waveform fits from the joint finite-fault inversion. | Nature Geoscience

Extended Data Fig. 5: Teleseismic waveform fits from the joint finite-fault inversion.

From: Seismic gap breached by the 2025 Mw 7.7 Mandalay (Myanmar) earthquake

Extended Data Fig. 5

Stations are shown in Figure S2. Gray and red lines show the filtered (0.05-0.2 Hz) observed and synthetic displacement waveforms, respectively. Black and red numbers in the top-left of each panel indicate the peak amplitudes (in cm) of the observed and synthetic traces. Light brown shading represents 500 synthetic waveform realizations sampled from the posterior distribution. Each trace is labeled with the station name and time (in minutes) relative to the origin time. Gray and orange histograms in the lower-left and upper-right corners show the station-specific time shifts and weighted variance reductions (VR), respectively; red lines indicate the maximum a posteriori (MAP) solution. The black histogram in the top-middle of each panel shows the weighted residuals.

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