What is she best known for?
The fields of study she is best known for:
- Volcano
- Plate tectonics
- Subduction
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
- Magma which is related to area like Graben, Rift and Interferometric synthetic aperture radar,
- Lava, which have a strong connection to Dense-rock equivalent and Lateral eruption.
The various areas that Sigrún Hreinsdóttir examines in her Asthenosphere study include Shear and Fault.
Her Episodic tremor and slip and Continental collision study in the realm of Subduction connects with subjects such as Neogene.
Her most cited work include:
- The 2002 Denali fault earthquake, Alaska: a large magnitude, slip-partitioned event. (317 citations)
- Intrusion triggering of the 2010 Eyjafjallajokull explosive eruption (294 citations)
- Segmented lateral dyke growth in a rifting event at Bárðarbunga volcanic system, Iceland (279 citations)
What are the main themes of her work throughout her whole career to date?
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
- Geophysics together with Explosive eruption,
- Geothermal gradient and related Subsidence.
Sigrún Hreinsdóttir interconnects Glacier, Tide gauge and Climate change in the investigation of issues within Geodesy.
Her Magma research is multidisciplinary, relying on both Inflow and Petrology.
She most often published in these fields:
- Seismology (65.82%)
- Volcano (41.77%)
- Geodesy (32.91%)
What were the highlights of her more recent work (between 2017-2021)?
- Seismology (65.82%)
- Volcano (41.77%)
- Interferometric synthetic aperture radar (12.66%)
In recent papers she was focusing on the following fields of study:
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.
Between 2017 and 2021, her most popular works were:
- Triggered Slow Slip and Afterslip on the Southern Hikurangi Subduction Zone Following the Kaikōura Earthquake (41 citations)
- Injection-induced surface deformation and seismicity at the Hellisheidi geothermal field, Iceland (17 citations)
- Geodynamics of Iceland and the signatures of plate spreading (14 citations)
In her most recent research, the most cited papers focused on:
- Volcano
- Plate tectonics
- Subduction
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.
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