Thomas Theunissen
Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, NorwayDistal margin formation
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
Seismic Modelling of Normal Faults
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 …
Underneath the volcano: Trying to understand how igneous sills are emplaced using outcrops and seismic from East Greenland Here I will tell you about our ongoing work to understand sill emplacement, using data from Jameson Land in East Greenland. …
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Relative continent/mid-ocean ridge elevation: a reference case for isostasy in geodynamics The choice on crustal and mantle densities in numerical geodynamics model is usually based on common habits. However, lithospheric deformation involving regional or fault-related flexure or involving strong change …