The Earth below ground is the subject of interest for many geophysical as well as geological
investigations. Even though most practitioners would agree that all available information …

We analytically evaluate the gravity anomaly associated with a polyhedral body having an
arbitrary geometrical shape and a polynomial density contrast in both the horizontal and …

Three-dimensional (3-D) interactive modeling permits integrated processing and
interpretation of gravity and magnetic data, yielding an improved geologic interpretation. 3-D …

The large scale structure of the earth is caused by geodynamic processes which are
explained using energetic, kinematic and dynamic descriptions. While" geodynamic …

An analytical solution is presented for the gravity anomaly produced by a 2D body whose
geometrical shape is arbitrary and where the density contrast is a polynomial function in …

We combine seismological and Bouguer anomaly data with thermo-kinematic and
petrological modelling to constrain the extent and kinetics of the eclogitization process in the …

A novel fast and accurate algorithm is developed for large‐scale 3‐D gravity and magnetic
modeling problems. An unstructured grid discretization is used to approximate sources with …

Investigation into understanding the genesis of brines in southeast Nigeria was carried out
utilizing high-resolution potential field (HRPF) data. This study reveals that igneous …

Three crustal-scale sequentially restored cross-sections along the Central External Betic
Cordillera enable us to pinpoint the role of extreme crustal thinning, tectonic inheritance and …

Back-arc basins are found at convergent plate boundaries. Nevertheless, they are zones of
significant crustal extension that show volcanic and hydrothermal processes somewhat …