2021
DOI: 10.1029/2020jb020157
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Ground Deformation After a Caldera Collapse: Contributions of Magma Inflow and Viscoelastic Response to the 2015–2018 Deformation Field Around Bárðarbunga, Iceland

Abstract: Ground deformation indicating volcano inflation, increase in seismic activity, changes in volcanic gas release, and thermal anomalies within a volcanic system are generally recognized as the indicators of volcanic unrest (e.g.,

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Cited by 13 publications
(28 citation statements)
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“…We use the semi-analytical software RELAX (Barbot & Fialko, 2010a, 2010b to calculate post-rifting displacement fields in response to the formation of a dike. We start with a two-layer Maxwell viscoelastic model, where a 7 km thick elastic layer lies on top of a 0.3 × 10 19 Pa s viscoelastic half-space, as described by Li et al (2021). Both layers consist of homogeneous isotropic material, with Poisson's ratio ν = 0.25 and shear modulus μ = 16 GPa (Grapenthin et al, 2006).…”
Section: Modeling and Resultsmentioning
confidence: 99%
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“…We use the semi-analytical software RELAX (Barbot & Fialko, 2010a, 2010b to calculate post-rifting displacement fields in response to the formation of a dike. We start with a two-layer Maxwell viscoelastic model, where a 7 km thick elastic layer lies on top of a 0.3 × 10 19 Pa s viscoelastic half-space, as described by Li et al (2021). Both layers consist of homogeneous isotropic material, with Poisson's ratio ν = 0.25 and shear modulus μ = 16 GPa (Grapenthin et al, 2006).…”
Section: Modeling and Resultsmentioning
confidence: 99%
“…We explore elastic layer thickness ranging from 1 to 24 km in steps of 1 km. As the displacement rate predicted by the viscoelastic model scales inversely with viscosity, we derive the result of different viscosities by scaling the displacement rate of the initial model, as done by Li et al (2021). We test viscosities in 0.1 × 10 19 Pa s steps from 0.3-3.6 × 10 19 Pa s.…”
Section: Modeling and Resultsmentioning
confidence: 99%
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