A 1D velocity model is a simplified representation of seismic wave velocities as a function of depth in the Earth, where the velocity is described as a single dimension over depth. This model is crucial for understanding how seismic waves travel through different geological layers, allowing for accurate predictions of travel times and wave propagation characteristics. The 1D aspect implies that variations in lateral dimensions are not considered, making it an idealized framework for initial analyses in seismology.
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