Seismic waves carry all the geological and geotechnical characteristics (fault, number of discontinuities, discontinuity direction, slope, rock quality, groundwater, etc.) of the units they pass along the route they travel on. Therefore, seismic waves can be called the signature of the route it passes through. Let's call the blasting point as the zero point (source). If the zero-point form of the blast-induced seismic waves measured at a certain distance from the zero point (on the target) can be revealed and this form can be integrated into the dynamic numerical model, the effects that will...