Seismic data are primarily used in studies of the Earth's inner structure. Since large parts of
the world are not yet sufficiently covered by seismic surveys, products from the Earth's …

In this work, we present a new gravimetric Moho model over the Gulf of Guinea computed
from the inversion of the global gravity EIGEN‐6C4 model. The computation procedure …

In this research, a modified form of Vening Meinesz-Moritz (VMM) theory of isostasy for the
second-order radial derivative of gravitational potential, measured from the Gravity field and …

The Moho surface can be determined according to isostatic theories, and among them, the
recent Vening Meinesz-Moritz (VMM) theory of isostasy has been successfully applied for …

Different approximations are used in Moho modelling based on isostatic theories. The well-
known approximation is considering a plate shell model for isostatic equilibrium, which is an …

One of the major issues associated with a regional Moho recovery from the gravity or gravity-
gradient data is the optimal choice of the mean compensation depth (ie, the mean Moho …

Subcrustal stress induced by mantle convection can be determined by the Earth's
gravitational potential. In this study, the spherical harmonic expansion of the simplified …

We develop a novel regional inversion algorithm to determinate the Moho geometry from the
gravity-gradient data. The procedure involves two steps. Firstly, the refined gravity-gradient …

Moho determination is an important issue in studying the Earth's interior structure. In
accordance with the isostasy-compensation hypothesis in geodesy, it is possible to recover …

The gravity field and steady-state ocean circulation explorer (GOCE) satellite mission has a
good global coverage of data except across the Polar Regions. Here, the goal is to take the …