The significance of the theorem in geophysical data processing lies in its ability to provide a mathematical framework for interpreting complex data sets. It facilitates the extraction of meaningful information from noise-dominated measurements, enhancing the accuracy of geological models. By applying this theorem, geophysicists can improve the resolution and reliability of subsurface imaging, leading to better resource exploration and environmental assessments. Ultimately, it helps bridge the gap between theoretical models and practical applications in the field.
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