Her scientific interests lie mostly in Seismology, Slip, Mantle, Moment magnitude scale and Lithosphere. Her Seismology study frequently draws connections between adjacent fields such as Crust. Sigrún Hreinsdóttir has included themes like Creep, Inlet and Viscoelasticity in her Slip study.
Her research on Caldera also deals with topics like
The scientist’s investigation covers issues in Seismology, Volcano, Geodesy, Deformation and Magma. Her research in Seismology intersects with topics in Slip, Crust and Interferometric synthetic aperture radar. Her work deals with themes such as Subduction and Episodic tremor and slip, which intersect with Slip.
Her Volcano study also includes fields such as
Her primary scientific interests are in Seismology, Volcano, Interferometric synthetic aperture radar, Deformation and Geothermal gradient. The study incorporates disciplines such as Slip and Anomaly in addition to Seismology. Explosive eruption is the focus of her Volcano research.
She studied Interferometric synthetic aperture radar and Caldera that intersect with Viscoelasticity. Her work carried out in the field of Deformation brings together such families of science as Induced seismicity and Magma. In her research, Mineralogy and Inlet is intimately related to Subsidence, which falls under the overarching field of Geothermal gradient.
Sigrún Hreinsdóttir focuses on Seismology, Deformation, Interferometric synthetic aperture radar, Geothermal power and Geothermal gradient. Her Seismology study frequently draws connections to adjacent fields such as Slip. Sigrún Hreinsdóttir combines subjects such as Volcano, Induced seismicity and Igneous rock with her study of Deformation.
Her Induced seismicity research is multidisciplinary, incorporating perspectives in Petrology, Volcanic hazards and Volcanic unrest, Magma. Her Interferometric synthetic aperture radar research includes themes of Post-glacial rebound, Rift and Caldera. Her Geothermal power investigation overlaps with other areas such as Geodesy, Subsidence, Pore water pressure, Volumetric flow rate and Crust.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
Complex multifault rupture during the 2016 Mw 7.8 Kaikōura earthquake, New Zealand
Ian J. Hamling;Sigrún Hreinsdóttir;Kate Clark;John Elliott.
The 2002 Denali fault earthquake, Alaska: a large magnitude, slip-partitioned event.
Donna Eberhart-Phillips;Peter J Haeussler;Jeffrey T Freymueller;Arthur D Frankel.
Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland
Freysteinn Sigmundsson;Andrew Hooper;Sigrún Hreinsdóttir;Kristín S. Vogfjörd.
Intrusion triggering of the 2010 Eyjafjallajokull explosive eruption
Freysteinn Sigmundsson;Sigrún Hreinsdóttir;Andrew Hooper;Thóra Árnadóttir.
Active Deformation Processes in Alaska, Based on 15 Years of GPS Measurements
Jeffrey T. Freymueller;Hilary Woodard;Steven C. Cohen;Ryan Cross.
Geophysical monograph (2013)
Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow
Magnús T. Gudmundsson;Kristín Jónsdóttir;Andrew Hooper;Eoghan P. Holohan.
Implications of deformation following the 2002 Denali, Alaska, earthquake for postseismic relaxation processes and lithospheric rheology
Andrew M. Freed;Roland Bürgmann;Eric Calais;Jeff Freymueller.
Journal of Geophysical Research (2006)
A large slow slip event and the depth of the seismogenic zone in the south central Alaska subduction zone
Yusaku Ohta;Jeffrey T. Freymueller;Sigrún Hreinsdóttir;Hisashi Suito.
Earth and Planetary Science Letters (2006)
Highly variable coastal deformation in the 2016 MW7.8 Kaikōura earthquake reflects rupture complexity along a transpressional plate boundary
K.J. Clark;E.K. Nissen;J.D. Howarth;I.J. Hamling.
Earth and Planetary Science Letters (2017)
Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge
Laura M. Wallace;Laura M. Wallace;Yoshihiro Kaneko;Sigrún Hreinsdóttir;Ian Hamling.
Nature Geoscience (2017)
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