Elías Rafn Heimisson
Elías Rafn Heimisson
Postdoctoral Scholar, ETH Zurich
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Cited by
Cited by
Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland
F Sigmundsson, A Hooper, S Hreinsdóttir, KS Vogfjörd, BG Ófeigsson, ...
Nature 517 (7533), 191-195, 2015
Kilometer‐scale Kaiser effect identified in Krafla volcano, Iceland
ER Heimisson, P Einarsson, F Sigmundsson, B Brandsdóttir
Geophysical Research Letters 42 (19), 7958-7965, 2015
Forecasting the path of a laterally propagating dike
ER Heimisson, A Hooper, F Sigmundsson
Journal of Geophysical Research: Solid Earth 120 (12), 8774-8792, 2015
Constitutive law for earthquake production based on rate‐and‐state friction: Dieterich 1994 revisited
ER Heimisson, P Segall
Journal of Geophysical Research: Solid Earth, 2018
Poroelastic effects destabilize mildly rate-strengthening friction to generate stable slow slip pulses
E Heimisson, EM Dunham, M Almquist
Journal of the Mechanics and Physics of Solids, 2019
Unexpected large eruptions from buoyant magma bodies within viscoelastic crust
F Sigmundsson, V Pinel, R Grapenthin, A Hooper, SA Halldórsson, ...
Nature communications 11 (1), 2403, 2020
Magma Movements in Volcanic Plumbing Systems and their Associated Ground Deformation and Seismic Patterns
F Sigmundsson, M Parks, R Pedersen, K Jónsdóttir, BG Ófeigsson, ...
Volcanic and Igneous Plumbing Systems, 285-322, 2018
Evolution of deformation and stress changes during the caldera collapse and dyking at Bárdarbunga, 2014–2015: Implication for triggering of seismicity at nearby …
MM Parks, ER Heimisson, F Sigmundsson, A Hooper, KS Vogfjörd, ...
Earth and Planetary Science Letters 462, 212-223, 2017
Crack to pulse transition and magnitude statistics during earthquake cycles on a self-similar rough fault
ER Heimisson
Earth and Planetary Science Letters, 2020
Ridgecrest aftershocks at Coso suppressed by thermal destressing
K Im, JP Avouac, ER Heimisson, D Elsworth
Nature 595 (7865), 70-74, 2021
Constitutive law for earthquake production based on rate‐and‐state friction: Theory and application of interacting sources
ER Heimisson
Journal of Geophysical Research: Solid Earth, 2019
Physically consistent modeling of dike induced deformation and seismicity: Application to the 2014 Bárðarbunga dike, Iceland
ER Heimisson, P Segall
Journal of Geophysical Research: Solid Earth, e2019JB018141, 2020
Dilatancy and compaction of a rate‐and‐state fault in a poroelastic medium: Linearized stability analysis
ER Heimisson, J Rudnicki, N Lapusta
Journal of Geophysical Research: Solid Earth 126 (8), e2021JB022071, 2021
Analytical prediction of seismicity rate due to tides and other oscillating stresses
ER Heimisson, JP Avouac
Geophysical Research Letters 47 (23), e2020GL090827, 2020
Stress-based forecasting of induced seismicity with instantaneous earthquake failure functions: applications to the Groningen Gas Reservoir
JD Smith, ER Heimisson, SJ Bourne, JP Avouac
Earth and Planetary Science Letters 594, 117697, 2022
Coulomb threshold rate-and-state model for fault reactivation: application to induced seismicity at Groningen
ER Heimisson, JD Smith, JP Avouac, SJ Bourne
Geophysical Journal International 228 (3), 2061-2072, 2022
A Spectral Boundary‐Integral Method for Faults and Fractures in a Poroelastic Solid: Simulations of a Rate‐and‐State Fault With Dilatancy, Compaction, and Fluid Injection
ER Heimisson, S Liu, N Lapusta, J Rudnicki
Journal of Geophysical Research: Solid Earth 127 (9), e2022JB024185, 2022
Logarithmic growth of dikes from a depressurizing magma chamber
BE Grossman‐Ponemon, ER Heimisson, AJ Lew, P Segall
Geophysical Research Letters, 2020
On the Integrated Surface Uplift for Dip‐Slip FaultsShort Note
P Segall, ER Heimisson
Bulletin of the Seismological Society of America, 2019
Deflation and deformation of the Askja caldera complex, Iceland, since 1983: Strain and stress development on caldera boundaries prior to tsunami generating rockslide in 2014 …
F Sigmundsson, V Drouin, M Parks, S Dumont, ER Heimisson, ...
AGU Fall Meeting Abstracts 2014, V51A-4715, 2014
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