[HTML][HTML] Structurally controlled rock slope deformation in northern Norway
Gravitational forcing of oversteepened rock mass leads to progressive failure, including
rupture, creeping, sliding and eventual avalanching of the unstable mass. As the point of …
rupture, creeping, sliding and eventual avalanching of the unstable mass. As the point of …
A new paradigm for large earthquakes in stable continental plate interiors
Large earthquakes within stable continental regions (SCR) show that significant amounts of
elastic strain can be released on geological structures far from plate boundary faults, where …
elastic strain can be released on geological structures far from plate boundary faults, where …
Postglacial relative sea level change in Norway
We present the first comprehensive postglacial relative sea-level (RSL) database for the
Norwegian coast from Oslo to the Kola Peninsula. The database spans the last 20 kyrs and …
Norwegian coast from Oslo to the Kola Peninsula. The database spans the last 20 kyrs and …
[HTML][HTML] Structural analysis of the Smeaheia fault block, a potential CO2 storage site, northern Horda Platform, North Sea
Smeaheia, a prominent fault block located on the Horda Platform, northern North Sea is
identified as a potential subsurface CO 2 storage site. We utilise the GN1101 3D seismic …
identified as a potential subsurface CO 2 storage site. We utilise the GN1101 3D seismic …
Evidence for the release of long‐term tectonic strain stored in continental interiors through intraplate earthquakes
TJ Craig, E Calais, L Fleitout… - Geophysical …, 2016 - Wiley Online Library
The occurrence of large earthquakes in stable continental interiors challenges the
applicability of the classical steady state “seismic cycle” model to such regions. Here we …
applicability of the classical steady state “seismic cycle” model to such regions. Here we …
Local seismicity and sediment deformation in the west Svalbard margin: Implications of neotectonics for seafloor seepage
P Domel, A Plaza‐Faverola… - Geochemistry …, 2023 - Wiley Online Library
Abstract In the Fram Strait, mid‐ocean ridge spreading is represented by the ultra‐slow
system of the Molloy Ridge, the Molloy Transform Fault and the Knipovich Ridge. Sediments …
system of the Molloy Ridge, the Molloy Transform Fault and the Knipovich Ridge. Sediments …
A comparison of strain rates and seismicity for Fennoscandia: depth dependency of deformation from glacial isostatic adjustment
M Keiding, C Kreemer, CD Lindholm… - Geophysical Journal …, 2015 - academic.oup.com
We investigate the influence of the glacial isostatic adjustment (GIA) on the deformation at
the surface and at seismogenic depths in Fennoscandia. The surface strain rate field …
the surface and at seismogenic depths in Fennoscandia. The surface strain rate field …
Probabilistic seismic hazard analysis in low-seismicity regions: an investigation of sensitivity with a focus on Finland
We investigate probabilistic seismic hazard analysis (PSHA) in low-seismicity regions in
which epistemic uncertainties are largely due to the sparsity of data, with a focus on Finland …
which epistemic uncertainties are largely due to the sparsity of data, with a focus on Finland …
To what extent is the present seismicity of Norway driven by post-glacial rebound?
The seismicity of Scandinavia is low to intermediate in intensity and with magnitudes that
rarely exceed 5.5. Even so, the seismicity is characterized by a great diversity in space and …
rarely exceed 5.5. Even so, the seismicity is characterized by a great diversity in space and …
Distribution and morphology of landslides in northern Finland: an analysis of postglacial seismic activity
The ages and sizes of landslides occurring in seismically active areas can be used to
reconstruct the seismic history of the area and estimate the maximum moment magnitudes of …
reconstruct the seismic history of the area and estimate the maximum moment magnitudes of …