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. 2024 Mar 21;14:6834. doi: 10.1038/s41598-024-55009-5

Figure 2.

Figure 2

Co-seismic rupture traces derived from co-seismic satellite displacements fields and field observations: (a) example of parallel to the fault displacements (computed along the direction of the EAF) at the junction of the Narli fault and the EAF; (b) gradient of the parallel to the fault displacements computed along profiles perpendicular to the direction of the EAF; (c) rupture traces (in black dots) derived from the gradient together with the rupture traces mapped by other authors6,39. The total fault zone width derived from the arctangent law (see Methods for more details) is shown in yellow; (d,f) are field pictures of the offset measured on the field at the intersection between the AA’ and BB’ profiles (Fig. 2a); (e,g) are examples of parallel-to-the fault displacement measurements from satellite image correlation (black dots) along the profiles AA’ and BB’. The measured rupture properties (i.e. total offset, on-fault offset and fault width) and the field measurements are represented together.