We developed and applied a novel numerical scheme for a gravimetric forward modelling of
the Earth's crustal density structures based entirely on methods for a spherical analysis and …

The principle of isostasy is important in different fields of geosciences. Using an isostatic
hypothesis for estimating the crustal thickness suffers from the more or less incomplete …

In the last years the scientific literature has been enriched with new models of the Moho
depth in the Antarctica Continent derived by the seismic reflection technique and refraction …

The geoid error, computed from EGM08, is unrealistically large due to the continuation of the
spherical harmonic coefficient errors down to the surface of the reference ellipsoid. In this …

Collocation approach has been applied to get a global Moho model in spherical
approximation based on a GOCE geopotential model. A simple single layer model, with …

The satellite gradiometry data (SGD) can be used for studying the crustal structure in
addition to the Earth's gravity field. This paper will show how this type of data is related to the …

We present a combined method for estimating a new global Moho model named KTH15C,
containing Moho depth and Moho density contrast (or shortly Moho parameters), from a …

We apply a newly developed numerical method to improve the Moho geometry by the
implementation of gravity data. This method utilizes expressions for the gravimetric forward …

The next-generation gravity satellite mission equipped with the Cold Atom Interferometry
(CAI) gradiometer has great potential for the Earth's gravity field estimation. Deploying a CAI …

The study of the discontinuity between crust and mantle beneath Iran is still an open issue in
the geophysical community due to its various tectonic features created by the collision …