The gravity anomalies reflect density perturbations at different depths, which control the
physical state and dynamics of the lithosphere and sub-lithospheric mantle. However, the …

We use the improved Parker‐Oldenburg's formulas that include a reference depth into the
exponential term and employ the Gauss‐fast Fourier transform method to determine Moho …

We develop a novel gravity inversion algorithm in spherical coordinates based on adaptive
inversion mesh refinement and multiphysical parameter constraints. The inversion mesh is …

The study and assessment of the subsurface density distribution are vital for mining and oil
and gas exploration. This can be achieved by the 3-D inversion of the observed gravity and …

In recent decades, colleagues working in the Discipline of Geological Resources and
Geological Engineering at Central South University made significant progress in theoretic …

The lunar mascon basins are characterized by high gravity anomalies and thin crust. Study
of the density structure beneath the mascon basins can help to understand the origin of …

Abstract The Gauss–Legendre quadrature (GLQ) integration is a numerical method to
calculate the gravitational field of a tesseroid and the approximation error of the GLQ …

Three-dimensional gravity inversion has been widely used to infer density structures and
tectonic movements of the earth and Moon. However, two problems (the nonuniqueness and …

The gravity gradient data have higher horizontal resolution and highlight the shallow
sources relative to gravity data; therefore, the comprehensive measurement of gravity and its …

To take the sphericity of the Earth into account, tesseroids are often utilized as grid elements
in large-scale gravitational forward modeling. However, such elements in a latitude …