Characteristics of Viscoelastic Crustal Deformation Following a Megathrust Earthquake: Discrepancy Between the Apparent and Intrinsic Relaxation Time Constants

• Published in: Pure and applied geophysics Vol. 175; no. 2; pp. 549 - 558
• Main Authors: Fukahata, Yukitoshi, Matsu’ura, Mitsuhiro
• Format: Journal Article
• Language: English
• Published: Cham Springer International Publishing 01.02.2018; Springer Nature B.V
• Subjects: Asthenosphere; Constants; Crustal deformation; Decay; Decay rate; Deformation; Deformation mechanisms; Earth and Environmental Science; Earth Sciences; Earthquakes; Elastic deformation; Elastic properties; Geophysics/Geodesy; Gravitation; Gravity; Half spaces; Lithosphere; Relaxation time; Seismic activity; Stress relaxation; Substrata; Surface boundary layer; Surface layers; Time; Time constant; Viscoelasticity; Wavelength; postseismic deformation; Viscoelastic relaxation; Maxwell time; megathrust earthquake
• DOI: 10.1007/s00024-017-1735-3
• ISSN: 0033-4553

The viscoelastic deformation of an elastic–viscoelastic composite system is significantly different from that of a simple viscoelastic medium. Here, we show that complicated transient deformation due to viscoelastic stress relaxation after a megathrust earthquake can occur even in a very simple situation, in which an elastic surface layer (lithosphere) is underlain by a viscoelastic substratum (asthenosphere) under gravity. Although the overall decay rate of the system is controlled by the intrinsic relaxation time constant of the asthenosphere, the apparent decay time constant at each observation point is significantly different from place to place and generally much longer than the intrinsic relaxation time constant of the asthenosphere. It is also not rare that the sense of displacement rate is reversed during the viscoelastic relaxation. If we do not bear these points in mind, we may draw false conclusions from observed deformation data. Such complicated transient behavior can be explained mathematically from the characteristics of viscoelastic solution: for an elastic–viscoelastic layered half-space, the viscoelastic solution is expressed as superposition of three decaying components with different relaxation time constants that depend on wavelength.