Physically consistent modeling of dike induced deformation and seismicity:  Application to the 2014 Bárðarbunga dike, Iceland

This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1029/2019JB018141.

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Authors

Elias Rafn Heimisson , Paul Segall

Abstract

Dike intrusions are often associated with surface deformation and propagating swarms of earthquakes.
These are understood to be manifestations of the same underlying physical process, although rarely modeled as such. We construct a physics-based model of the 2014 B\ar{\dh}arbunga dike, by far the best observed large dike ($> 0.5$ km$^3$) to date. We constrain the background stress state by the total dike deformation, the time-dependent dike pressure from continuous GPS and the extent of the seismic swarm, and the spatial dependence of frictional properties via the space-time evolution of seismicity. We find that the geodetic and earthquake data can be reconciled with a self-consistent set of parameters. The complex spatial and temporal evolution of the B\ar{\dh}arbunga seismicity can be explained by dike-induced elastic stress changes on preexisting faults, constrained by observed focal mechanisms. In particular, the model captures the segmentation of seismicity, where only the newest dike segment is seismically active. Our results indicate that many features of the seismicity result from the interplay between time-dependent magma pressure within the dike and stress memory effects. The spatial variability in seismicity requires heterogeneity in frictional properties and/or local initial stresses. Modeling suggests that the dike pressure drops during rapid advances and increases during pauses, which primarily causes the segmentation of the seismicity. Joint analysis of multiple data types could potentially lead to improved, physics-based eruption forecasts.

DOI

https://doi.org/10.31223/osf.io/fdv8h

Subjects

Earth Sciences, Geology, Geophysics and Seismology, Physical Sciences and Mathematics, Volcanology

Keywords

rate-and-state friction, Seismicity, dike propagation, joint inversion, magmatic intrusions

Dates

Published: 2019-06-03 13:52

Last Updated: 2020-01-27 17:49

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License

CC BY Attribution 4.0 International

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