The global crustal model CRUST1. 0 (refined using additional global datasets of the solid
topography, polar ice sheets and geoid) is used in this study to estimate the average …

The latest seismic data and improved information about the subglacial bedrock relief are
used in this study to estimate the sediment and crustal thickness under the Antarctic …

The boundary between Earth's crust and mantle is commonly modelled as a discontinuity
surface, the so-called Moho. Although in some regions of the world this model may be too …

The discontinuity surface between Earth crust and mantle, the so-called Moho, is commonly
estimated by means of seismic or gravimetric methods. Usually these methods do not yield …

Abstract Based on Vening Meinez-Moritz global inverse isostatic problem, the Moho density
contrast is formulated as that of finding a solution of a Fredholm integral equation of the first …

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 …

The present study attempts a conjugate analysis of satellite-based remote sensing, gravity,
and magnetic data for evaluation of structures and tectonic for new insights on Kimberlite …

Two hyperparameters, the mean Moho depth and the Moho density contrast, must be
specified before the gravity inversion of Moho. Incorrect estimation will impact inversed …

We analyse spatial and spectral characteristics of various refined gravity data used for
modelling and gravimetric interpretation of the crust–mantle interface and the mantle …

From the 2000s onwards, unprecedented space missions have brought about a wealth of
novel investigations on the different aspects of space geomechanics. Such aspects are …