This disclosure relates to the field of
geological structure assessment technology, and particularly to a method, apparatus, equipment, medium, and
computer program for determining strike-slip displacement. The method includes performing the following determination process on both the first and second strata located on both sides of the target
fault plane: determining the uplift area and depth of the strata corresponding to the
gypsum-salt development area; determining the strata shortening based on the uplift area and depth; and determining the strike-slip displacement of the target
fault plane based on the strata shortening corresponding to the first and second strata. For the first and second strata, the uplift area and depth of the strata corresponding to the
gypsum-salt development area are used as the basis for determining the strata shortening. Utilizing
gypsum-salt rheological theory, the kinematic characteristics of the gypsum-salt development area are extracted and the strata shortening is determined according to their established correspondence, thereby simplifying the strike-slip displacement determination process and ensuring the accuracy of the strike-slip displacement determination results.