Seismic Wave Equation, Ray Tracing, and Wavefront Tracking with Code Implementation
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Detailed Documentation
Seismic wave equation, ray tracing, and wavefront tracking are widely used techniques in seismology. These methods enable researchers to study and analyze the propagation patterns and characteristics of seismic waves through various media. Ray tracing, implemented through algorithms like shooting or bending methods, calculates seismic wave propagation paths and travel times through complex geological structures. Wavefront tracking represents a more advanced technique that simulates the entire wave propagation process, including diffraction, reflection, and refraction phenomena in heterogeneous media using finite-difference or spectral element methods. Additional documentation and constant-gradient ray tracing methods for complex media are essential tools in seismological research, helping seismologists better understand and interpret seismic wave propagation mechanisms through numerical modeling approaches.
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