Earthquakes track subduction fluids from slab source to mantle wedge sink Felix Halpaap1, Stéphane Rondenay1, Alexander Perrin2, Saskia Goes2, Lars Ottemöller1, Florian Millet1,3, Håkon Austrheim4, Robert Shaw2 and Thomas Eeken2 1) Department of Earth Science, University of Bergen, …
Supra-detachment basin - Norwegian passive margin
The European Plate Observing System portal
4 AGU practice talks: Helene Meling Stemland | Applications of surface seismic on thawing saline permafrost: examples from the Norwegian Arctic Anneleen H. Geurts | Drainage integration in active continental rifts: tipping the balance between basin filling and subsidence Hasbi Ash …
Electromagnetic modelling and inversion using integral equation methods
Detrital zircon inventory of the Triassic Greater Barents Sea Basin: sediment transport and geodynamics Hallgeir Sirevaag, Christian Haug Eide, Albina Gilmullina, Leif-Erik Rydland Pedersen The intra-cratonic Greater Barents Sea Basin (GBSB) represents one of the last underexplored petroleum provinces in …
How does topography evolve during growth and decay of a mountain belt - inferences from coupled tectonic-surface process models It has been a long-standing problem how mountain belts gain and loose topography during their tectonically active growth and inactive decay …
Increasing fault-slip rates within the Corinth Rift: A localising active rift fault network The young (<5 Ma) and active Corinth Rift, Greece, is one of the fastest extending rift zones in the world with present day extension rates of up …