Asymptotic co- and post-seismic displacements in a homogeneous Maxwell sphere. Issue 1 (1st May 2018)

• Record Type: Journal Article
• Authors: Tang, He; Sun, Wenke
• Is Part Of: Geophysical journal international. Volume 214:Issue 1(2018:Jul.)
• Page Start: 731
• Page End: 750
• Publication Date: 2018-05-01
• Subjects: Seismic cycle -- Transient deformation -- Theoretical seismology; Geophysics -- Periodicals; 550
• DOI: 10.1093/gji/ggy174
• Languages: English
• ISSNs: 0956-540X

Abstract

SUMMARY: The deformations of the Earth caused by internal and external forces are usually expressed through Green's functions or the superposition of normal modes, that is, via numerical methods, which are applicable for computing both co- and post-seismic deformations. It is difficult to express these deformations in an analytical form, even for a uniform viscoelastic sphere. In this study, we present a set of asymptotic solutions for computing co- and post-seismic displacements; these solutions can be further applied to solving co- and post-seismic geoid, gravity and strain changes. Expressions are derived for a uniform Maxwell Earth by combining the reciprocity theorem, which links earthquake, tidal, shear and loading deformations, with the asymptotic solutions of these three external forces (tidal, shear and loading) and analytical inverse Laplace transformation formulae. Since the asymptotic solutions are given in a purely analytical form without series summations or extra convergence skills, they can be practically applied in an efficient way, especially when computing post-seismic deformations and glacial isotactic adjustments of the Earth over long timescales.