One-Dimensional Gravity Forward Modeling and Least Squares Inversion

This geophysical exploration method employs one-dimensional gravity forward modeling and least squares inversion techniques to measure gravity anomalies caused by geological bodies with density contrasts to surrounding rocks. It determines their spatial positions, sizes, and shapes, enabling assessments of geological structures and mineral distributions in survey areas. The implementation typically involves modeling subsurface density variations using kernel functions and solving inverse problems through iterative optimization algorithms.