• Melanie Kling

    Response of a clastic source-to-sink system to extreme environmental perturbations: the Permian-Triassic transition on Finnmark Platform, Barents Sea Melanie Kling The eruption of the Siberian Traps at the Permian-Triassic transition significantly affected depositional environments world-wide. Known consequences are (I) extreme …

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  • Martin Kjenes

    Martin Kjenes coming soon...

  • Helene Stemland

    Helene Stemland coming soon...

  • James Opemipo Olomo

    Along strike variability of structural style and evolution of the South Viking Graben and western flank of the Utsira High James Opemipo Olomo      

  • Mads Jelby

    Far from home: Facies architecture of distal delta wedges across a wide ramp (Lower Cretaceous, Svalbard) Mads E. Jelby

  • Anne Imig

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

    Assessing managed aquifer recharge as a sustainable measure for groundwater management – An application for Grand Bahama Anne Imig A large storm surge caused by Hurricane Dorian in 2019 resulted in saltwater intrusion into the aquifers of Grand Bahama Island. …

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  • Enry Horas Sihombing

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

    Geomorphology of normal fault footwalls and fault scarps: Greater Tampen Spur Area, northern North Sea Enry Horas Sihombing Late Jurassic rifting in the Greater Tampen Spur area created a network of major normal faults, the footwall crests and fault scarps …

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  • Kui Xang

    Non-linear inverse scattering in anisotropic elastic media using a modified Born iterative method Kui Xang Estimating an accurate subsurface model of the Earth is crucial for identifying the locations of reservoirs. With the development of long offsets and wide azimuth …

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  • Dana Silerova

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

    Long-lived (180 Myr) ductile flow within the Great Slave Lake shear zone Dana Silerova The Great Slave Lake shear zone (GSLsz) is a type example for deeply eroded continental transform boundaries located in the Northwest Territories, Canada. Formed during the …

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