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Surface faulting and distribution of surface deformation caused by the Chirpan (M6.8) and Plovdiv (M7.0) earthquakes that occurred on 14 and 18 April 1928, respectively, were used with the scope to determine the distribution of slip and confirm the fault geometry. We assumed smooth fault geometry, based on previous studies, and a standard dislocation model. The faulting zone comprises several fault segments with different slip on each of them. For structurally complex areas like our study area the best model may b...