Hamed Khani

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

Pre-Mesozoic structural configuration in the northern North Sea rift basin; as a result of Devonian orogenic collapse in the Scandinavian-Scottish Caledonides The northern North Sea rift basin is a product of multiple rifting phases during the Mesozoic time, developed on …

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Gang Lu

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

Potential temperature and margin width control melt volume at rifted margins Gang Lu and Ritske S. Huismans Passive continental margins may have a wide variety of structural and magmatim styles, but the controlling factors of magmatism remain controversial. Common explanations …

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Anna Ksienzyk

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

Post-Caledonian fault activity in W-Norway: onshore and offshore don’t match – or do they? by Ksienzyk, A.K., Wemmer, K., Rotevatn, A., Fazlikhani, H., Jacobs, J., Fossen, H. K-Ar or Ar-Ar analyses of fault gouge fine fractions are becoming well-established methods …

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Thilo Wrona

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

Silica diagenesis and physical properties of Cenozoic rocks in the North Viking Graben, northern North Sea by Thilo Wrona, Christopher A-L. Jackson, Mads Huuse and Kevin G. Taylor As an introduction, I thought it would be nice to present some …

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Thomas Theunissen

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

Long-term coupling and feedbacks between surface processes and tectonics during rifting Whereas significant efforts have been made to understand the feedback between mountain building and surfaces processes, limited research has been done on the relationship between surface processes and extensional tectonics. …

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Vivi Pedersen

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

Inverse modeling of Eocene to mid-Pliocene landscape evolution in Scandinavia using offshore sediment volumes The origin of high topography in Scandinavia is highly debated, both in terms of its age and the underlying mechanism for its formation. Traditionally, the current …

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Anna Ksienzyk

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

Digital field assistant – teaching structural geology by mobile device Anna K. Ksienzyk, Christian Rønnevik, Joachim Jacobs & Hallgeir Sirevaag University of Bergen, Department of Earth Science, P. O. Box 7803, 5020 Bergen, Norway; anna.ksienzyk@uib.no, cronnevik@gmail.com, joachim.jacobs@uib.no, hallgeir.sirevaag@uib.no Rising student numbers present a challenge …

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Hongliang Wang

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

Water migration in the subduction mantle wedge: a two-phase flow approach Hongliang Wang, Ritske S. Huismans, and Stéphane Rondenay   Subduction zones are the main entry points of water into earth’s mantle and play an important role in the global …

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Benjamin Bellwald

Modeling potential paleoearthquakes based on results from subaquatic mass movements in Western Norway During my PhD as a Quaternary geologist, I did quite some work on turbidite paleoseimology in west- and mid-Norway, with some very interesting outcomings. I was further …

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