Numerical modeling study demonstrates efficient matrix-free gravity and magnetic inversion over complex topography, highlighting reduced memory demands and accurate subsurface density recovery.
To address the difficulty of terrain representation and the high storage cost of explicit sensitivity matrices in three-dimensional gravity and magnetic modeling and inversion, we propose a matrix-free framework based on terrain-conforming unstructured hexahedral meshes. Irregular topography is represented using eight-node deformed hexahedral elements, and element integrals are evaluated through isoparametric mapping and Gaussian quadrature. Precomputed Gaussian-point coordinates and Jacobian weights are shared by the forward and adjoint operators, enabling matrix-free evaluation of forward responses, adjoint actions, and Hessian–vector products without storing the full sensitivity matrix. An anomaly- and topography-guided adaptive parameterization further reduces the number of model parameters and Gaussian source points. Synthetic tests demonstrate numerical consistency with the conventional explicit-matrix method, substantial reductions in computation time and memory usage, and stable accuracy under pronounced terrain relief. Application to gravity data from the San Nicolás deposit recovers high-density anomalies consistent with the known massive sulfide body, confirming the effectiveness of the proposed method in complex terrain.
No takes yet. Share an insight, caveat, or question.
Jia et al. (2026) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: