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Elías Rafn Heimisson - Rannsóknalektor

Elías Rafn Heimisson

–

Verkfræði- og náttúruvísindasvið

Elías Rafn Heimisson

Rannsóknalektor

Sérfræðingur

Aðsetur
Askja / N-327
Sími
5254642 6939188
Tölvupóstur
eliasrafn [hjá] hi.is

Starfseining
Jarðvísindastofnun

ORCID vefsíða
https://orcid.org/0000-0001-8342-7226
Rannsóknagátt – Elías Rafn Heimisson

Show Útgefið efni

2025

Applying and validating Coulomb rate-and-state seismicity models in acoustic emission experimentsTectonophysics
Poroelastic effects on rupture propagation across fault stepoversEarth and Planetary Science Letters

2024

A coupled finite difference-spectral boundary integral method with applications to fluid diffusion in fault structuresInternational Journal for Numerical and Analytical Methods in Geomechanics
Analytical boundary integral solutions for cracks and thin fluid-filled layers in a 3D poroelastic solid in time and wavenumber domainJournal of the Mechanics and Physics of Solids
Modeling dike trajectories in a biaxial stress field with coupled magma flow, fracture, and elasticityBulletin of Volcanology

2023

The role of three-dimensional fault interactions in creating complex seismic sequencesEarth and Planetary Science Letters

2022

A Spectral Boundary-Integral Method for Faults and Fractures in a Poroelastic SolidJournal of Geophysical Research: Solid Earth
Coulomb threshold rate-and-state model for fault reactivationGeophysical Journal International
Spectral boundary integral method for simulating static and dynamic fields from a fault rupture in a poroelastodynamic solidGeomechanics and Geophysics for Geo-Energy and Geo-Resources
Stress-based forecasting of induced seismicity with instantaneous earthquake failure functionsEarth and Planetary Science Letters

2021

Dilatancy and Compaction of a Rate-and-State Fault in a Poroelastic MediumJournal of Geophysical Research: Solid Earth
Ridgecrest aftershocks at Coso suppressed by thermal destressingNature

2020

Analytical Prediction of Seismicity Rate Due to Tides and Other Oscillating StressesGeophysical Research Letters
Crack to pulse transition and magnitude statistics during earthquake cycles on a self-similar rough faultEarth and Planetary Science Letters
Logarithmic Growth of Dikes From a Depressurizing Magma ChamberGeophysical Research Letters
Physically Consistent Modeling of Dike-Induced Deformation and SeismicityJournal of Geophysical Research: Solid Earth
Unexpected large eruptions from buoyant magma bodies within viscoelastic crustNature Communications

2019

Constitutive Law for Earthquake Production Based on Rate-and-State FrictionJournal of Geophysical Research: Solid Earth
Poroelastic effects destabilize mildly rate-strengthening friction to generate stable slow slip pulsesJournal of the Mechanics and Physics of Solids
Short note on the integrated surface uplift for dip-slip faultsBulletin of the Seismological Society of America

2018

Constitutive Law for Earthquake Production Based on Rate-and-State FrictionJournal of Geophysical Research: Solid Earth
Magma movements in volcanic plumbing systems and their associated ground deformation and seismic patterns

2017

Evolution of deformation and stress changes during the caldera collapse and dyking at Bárdarbunga, 2014–2015Earth and Planetary Science Letters

2015

Forecasting the path of a laterally propagating dikeJournal of Geophysical Research: Solid Earth
Kilometer-scale Kaiser effect identified in Krafla volcano, IcelandGeophysical Research Letters

2014

Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, IcelandNature

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