Jan Michalek
Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, NorwayThe European Plate Observing System portal
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 …
High in the sky: geology and flying Atle Rotevatn, who in addition to being a professor in our department is also well into his training to become a pilot (PPL-A for those familiar with flying). In this talk he will …
Crustal Structure of Nordland: a preliminary result from seismic tomography Nordland is the most seismically active region in mainland Norway. Historically, the 1819 Lurøy / Rana earthquake (magnitude estimate 5.8 – 6.0) was the largest earthquake in northern Europe for …
Assessing First-order BQART Estimates for Ancient Source-to-Sink Mass Budget Calculations: The Sognefjord Source-to-Sink system, Northern North Sea Rift. Constraining the timing and volume of sediment dispersal in an ancient sedimentary system is vital to understand a basins infill history. In …
Distal margin formation