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Updated: Dec 15, 2025

Studying Large Amplitude Oscillatory Shear Response of Soft Materials
Published on: April 25, 2019
A linear viscoelasticity for decadal to centennial time scale mantle deformation
E R Ivins1, L Caron1, S Adhikari1
1Jet Propulsion Lab, California Institute of Technology, 4800 Oak Grove Dr., Pasadena, CA, 91109.
The extended Burgers material (EBM) model, a linear viscoelastic theory, is crucial for understanding rock deformation. Its parameters are vital for interpreting seismic data, planetary tides, and post-seismic relaxation, impacting geodetic studies of crustal motion.
Area of Science:
- Geophysics
- Solid Earth Science
- Rheology
Background:
- The extended Burgers material (EBM) model is a linear viscoelastic theory used in geophysics.
- It is important for parameterizing laboratory data, interpreting seismic wave velocity and attenuation, and analyzing planetary tidal dispersion and quality factor Q.
- The model assumes a distribution of relaxation spectra linked to rock grain boundary and interior granular mobility, with Maxwellian long-term behavior.
Purpose of the Study:
- To isolate parameters of the EBM that are applicable to post-seismic relaxation processes in the upper mantle and tidal studies.
- To investigate the influence of EBM transient rheology on geodetic interpretations of crustal motions induced by unloading.
Main Methods:
- Utilized the linear theory of viscoelasticity to isolate EBM parameters.
- Applied analytical Laplace transformed solutions of Boussinesq's half-space load problem.
Main Results:
- Identified EBM parameters relevant to post-seismic relaxation and tidal studies.
- Demonstrated that EBM transient rheology significantly impacts geodetic interpretations of unloading-induced crustal motions, even on sub-decadal timescales.
Conclusions:
- The isolated EBM parameters are applicable to post-seismic relaxation, tidal studies, and glacial isostatic adjustment.
- EBM provides a robust framework for understanding complex rock deformation phenomena across various geophysical applications.
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