Atle Rotevatn

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

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 …

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Hasbi Ash Shiddiqi

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

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 …

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Björn Nyberg

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

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 …

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Thomas Theunissen

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Distal margin formation

Lorenz Michel

The usual place Room 2G16c, 2nd floor, Realfabyyget, 41 Allégaten, Bergen, Norway

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 …

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Gang Lu

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Rifting models with magmatism

EGU practice talks

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Kui Xiang

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Seismic Waveform Modelling

Vilde Dimmen

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Seismic Modelling of Normal Faults

Christopher Jackson

Hot rocks under our feet; seismic reflection imaging of the processes and products of crustal magmatism Volcanoes are hot, loud and scary, thus we know little of their internal structure or underlying 'plumbing systems'. Magma intrusion in the Earth's crust, and …

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