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
Investigating feedbacks between tectonics and earth surface processes during rifting and continental breakup Disentangling the interactions and possible feedbacks between tectonic and earth surface processes has been a focus of geoscientific research. Many previous studies were conducted in convergent settings …
Rifting models with magmatism
Seismic Waveform Modelling