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During the exploration of earthquakes, one of the most commonly used methods is the finite difference method for simulating wavefield forward modeling. This method employs a simple layered model as its model for analysis. The reason for using the finite difference method is that it is a numerical method for solving differential equations. In the case of seismic exploration, the differential equation represents the wave equation, which describes the propagation of waves in the subsurface. The finite difference method is also used because it is a relatively simple and efficient way to solve the wave equation and to simulate wave propagation. By using this method, the geophysicists can better understand the structure of the subsurface and locate potential areas of interest for further exploration.