A generalized theory of the figures of the Earth's interior to a third-order precision of ellipticity is proposed in accompanying paper in which all the odd degree and nonzero order spherical harmonic terms are included. As both the direct and indirect contributions of the asymmetric crust are included, this theory makes a significant improvement for calculating the asymmetric equilibrium figures of the real Earth comparing with the traditional theories which can only deal with the ideal symmetric Earth. The principal moments of inertia (PMOI: A, B, C) and global dynamical flattening (H) are important quantities in studying the rotating Earth. Precession and gravity observations give observation value of H (Hobs approximate to 1/305.4559) w...
International audienceThe dynamical ellipticity of a planet expresses the departure of its mass dist...
After describing all the contradictions associated with the current Plate Tectonics theory, this pap...
We use the CRUST 2.0 crustal model and the EGM08 geopotential model to compile global maps of the gr...
Traditionally a laterally homogeneous and spherical base Earth model (e.g., the PREM model) is consi...
By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotatin...
From the observed precession of the equator, the luni-solar precession can be deduced by accounting ...
Different mass distributions within the lithosphere and the asthenosphere have been here considered ...
Abstract:Equatorial flattening of the core were previously estimated to be 5 × 10−4 by using seismic...
In this research, we computed the nutation of the figure axis for a non-rigid Earth model due to the...
The knowledge of the gravitational potential coefficients J(2) and J(4) of a hydrostatic Earth model...
On the basis of a new concept of reverse gravity operated in the Earth’s deep interior caused by the...
We determine the deformation produced by the lunisolar tidal potential in a rotating, spheroidal mod...
International audienceThe knowledge of the gravitational potential coefficients J2 and J4 of a hydro...
The boundary between Earth's crust and mantle is commonly modelled as a discontinuity surface, the s...
Equatorial flattening of the core were previously estimated to be 5 × 10−4 by using seismically deri...
International audienceThe dynamical ellipticity of a planet expresses the departure of its mass dist...
After describing all the contradictions associated with the current Plate Tectonics theory, this pap...
We use the CRUST 2.0 crustal model and the EGM08 geopotential model to compile global maps of the gr...
Traditionally a laterally homogeneous and spherical base Earth model (e.g., the PREM model) is consi...
By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotatin...
From the observed precession of the equator, the luni-solar precession can be deduced by accounting ...
Different mass distributions within the lithosphere and the asthenosphere have been here considered ...
Abstract:Equatorial flattening of the core were previously estimated to be 5 × 10−4 by using seismic...
In this research, we computed the nutation of the figure axis for a non-rigid Earth model due to the...
The knowledge of the gravitational potential coefficients J(2) and J(4) of a hydrostatic Earth model...
On the basis of a new concept of reverse gravity operated in the Earth’s deep interior caused by the...
We determine the deformation produced by the lunisolar tidal potential in a rotating, spheroidal mod...
International audienceThe knowledge of the gravitational potential coefficients J2 and J4 of a hydro...
The boundary between Earth's crust and mantle is commonly modelled as a discontinuity surface, the s...
Equatorial flattening of the core were previously estimated to be 5 × 10−4 by using seismically deri...
International audienceThe dynamical ellipticity of a planet expresses the departure of its mass dist...
After describing all the contradictions associated with the current Plate Tectonics theory, this pap...
We use the CRUST 2.0 crustal model and the EGM08 geopotential model to compile global maps of the gr...