By far the most prescient insights into the interior structure of the planet have been provided
on the basis of elastic wave seismology. Analysis of the travel times of shear or compression …

Summary The M w γ 9.0 2004 December 26 Sumatra-Andaman and M w= 8.7 2005 March
28 Nias earthquakes, which collectively ruptured approximately 1800 km of the Andaman …

The Andrade rheological model is often employed to describe the response of solar system
or extra‐solar planets to tidal perturbations, especially when their properties are still poorly …

Post-seismic deformation caused by the 2004 Sumatra-Andaman Earthquake (M= 9.3) has
been observed by space geodetic techniques such as the Global Positioning System (GPS) …

The choice of the physical model of postglacial rebound plays a decisive role to derive
information about the mantle rheology and viscosity from observed data. In models for the …

This paper presents a method that modifies commercial engineering-oriented finite element
packages for the modelling of Glacial Isostatic Adjustment (GIA) on a self-gravitating …

A homogeneous or stratified viscoelastic half-space has often been used as a simple earth
model to calculate the deformation induced by an earthquake or a regional deglaciation …

ALMA is a Fortran 90 program for computing the tidal and the loading “Love numbers” of a
spherically symmetric, incompressible, viscoelastic planet, using the Post–Widder Laplace …

Significant land uplift and horizontal motions have been recorded with Global Navigation
Satellite Systems (GNSS) in areas such as Alaska, Iceland and the Northern Antarctic …

Recently, Purcell has discussed the influence of gravity on load-induced perturbations of
compressible, viscoelastic plane-Earth models, where the contributions arising from initial …