Geophysical inversion is a mathematical and computational technique used to deduce subsurface properties from surface measurements, effectively reversing the process of forward modeling. This technique is crucial in transforming observed data, such as seismic waves or electromagnetic fields, into meaningful information about the geological structure and properties of the Earth's interior. By utilizing forward models to predict data, inversion allows for the refinement and adjustment of these predictions based on real-world observations, thereby enabling better understanding and characterization of subsurface resources.
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