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The postseismic InSAR deformation fields (a–h), the postseismic GPS horizontal displacement (c), and (i–l) the time series of typical deformation points. The dashed black lines AA’–DD’ indicate the profile in Figure S3a–d. The black boxes labeled as a-d in (c,g) indicate specifically selected points in (i–l). The black dashed curve represents the isopleth with a 5 mm interval, and Figure 9a,b are overlaid as isopleth in (c) and (g), respectively. The black arrow in subgraph (c) indicates the postseismic GPS horizontal displacement in the current period. F6 represents the fault that was reactivated by the Maduo event. The coarse grey curves in (i–l) represent the best-fit curve (see Formula (2)), and the values of the decay coefficient (τ, unit in day) are labeled near the curves. The red star shows the relocated epicenter.

The postseismic InSAR deformation fields (a–h), the postseismic GPS horizontal displacement (c), and (i–l) the time series of typical deformation points. The dashed black lines AA’–DD’ indicate the profile in Figure S3a–d. The black boxes labeled as a-d in (c,g) indicate specifically selected points in (i–l). The black dashed curve represents the isopleth with a 5 mm interval, and Figure 9a,b are overlaid as isopleth in (c) and (g), respectively. The black arrow in subgraph (c) indicates the postseismic GPS horizontal displacement in the current period. F6 represents the fault that was reactivated by the Maduo event. The coarse grey curves in (i–l) represent the best-fit curve (see Formula (2)), and the values of the decay coefficient (τ, unit in day) are labeled near the curves. The red star shows the relocated epicenter.

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Exploring the deformation mechanism of the 2021 Mw 7.4 Maduo Earthquake is crucial for better understanding the seismic hazard of the faults with low strain rates inside the Bayan Har block. This study leverages deformation information derived from Sentient-1 A/B images and GPS data to investigate in detail the co- and postseismic deformation mecha...

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