• 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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  • Christian Haug Eide

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

    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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  • Hasbi Ash Shiddiqi

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

    More details soon !

  • Thomas Theunissen

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

    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 …

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