The Green's function (GF) method, which makes use of GFs, is an important and elegant tool
for solving a given boundary-value problem for the differential equation from a real …

Temporal variations of surface masses, such as the hydrosphere and atmosphere of the
Earth, load the surfaces of planetary bodies causing temporal variations in deformation …

In this paper, we derive analytical expressions for the dislocation Love numbers (DLNs) for a
layered, spherical, transversely isotropic and self-gravitating Earth. This solution is based on …

We derive exact asymptotic solutions for the static deformation due to a concentrated or
point-like dislocation in a spherical, layered, elastic, isotropic and self-gravitating Earth. The …

We present an accurate approach for calculating the point-dislocation Green's functions
(GFs) for a layered, spherical, transversely-isotropic and self-gravitating Earth. The …

In this paper, we derive analytical solutions for the dislocation Love numbers (DLNs) and the
corresponding Green's functions (GFs) within a layered, spherical, transversely isotropic and …

Computing theoretical seismograms from a point source in a given Earth model is essential
for modeling and inversion of observed seismic waveforms for Earth's structure and …

We review the theory of the Earth's elastic and gravitational response to a surface disk load.
The solutions for displacement of the surface and the geoid are developed using …

Pan et al. presented a new analytical approach to compute the elastic load Love numbers
(ELLNs) for an elastic, transversely isotropic, spherical, layered and self-gravitating Earth …

Using a numerical integral method, we deduced a set of formulae for the co-seismic internal
deformation in a spherically symmetric earth model, simultaneously taking self-gravitation …