Seismology
The common midpoint (CMP) is a key concept in seismic refraction and reflection methods that refers to a point on the surface where seismic waves from two or more sources converge. This point is critical for accurately processing and interpreting seismic data, as it allows for the generation of symmetrical wave patterns that facilitate the analysis of subsurface structures. The use of CMP helps in enhancing the clarity and resolution of seismic images, which is essential for identifying geological features and potential resources.
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