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 …

Density variations drive mass transport in the Earth from plate tectonics to convection in the
mantle and core. Nevertheless, density remains poorly known because most geophysical …

We modeled crustal and lithospheric thickness variation as well as the variations in
temperature, composition, S wave seismic velocity, and density of the lithosphere beneath …

To solve the inverse gravimetric problem, ie, to estimate the mass density distribution that
generates a certain gravitational field, at local or regional scale, several parameters have to …

This paper presents the setup and pressure calibration of an 800-ton multi-anvil apparatus
installed at the Vrije Universiteit (Amsterdam, the Netherlands) to simulate pressure …

The evolution of the Philippine Sea Plate (PSP) since Jurassic is one of the key issues in the
dynamics of lithosphere and mantle. The related studies benefited mostly from seismic …

In this work, we study the lithospheric structure of the British Isles using a methodology that
allows for forward modeling of the Curie temperature depth based on seismic, elevation and …

Density perturbations in the subsurface are the main driver of mantle convection and can
contribute to lithospheric deformation. However, in many places the density structure in the …

A 3D density structure of the lithosphere and upper mantle beneath the eastern
Mediterranean Sea (EMS) and its adjacent region was constructed based on gravity …

Current seismic tomography models show a complex environment underneath the crust,
corroborated by high-precision satellite gravity observations. Both data sets are used to …