• Hongliang Wang

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

    A two-stage thickening and stabilization model for the formation of cratonic lithosphere Hongliang Wang (UiB) How Archaean tectonics was capable of producing virtually indestructible cratonic lithosphere remains a topic of considerable debate.  Recent geophysical and petrological studies refuelled the debate by …

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  • Luigia Cristiano

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

    Automated determination of P-wave polarization at GRSN Luigia Cristiano (1), Thomas Meier (1), Christian Weidle (1), and Frank Krüger (2) (1) Christian-Albrechts Universität, Kiel, Germany (luigia@geophysik.uni-kiel.de), (2) Universität Potsdam, Potsdam, Germany Body wave traveltimes are often analyzed for the investigation …

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  • Jan Michalek

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

    Seismicity of the Nordland area, Norway Jan Michalek University of Bergen  ABSTRACT: The Nordland area (65-70N; 8-18E) is tectonically active part of Norway. Enhanced seismicity may reflect on off-shore subsidence combined with the uplift of landmasses usually attributed to glacial …

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  • Kathrin Spieker

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

    TITLE: Moho depth variations beneath the Azores Islands  

  • David Peacock

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

    Fault interactions and associated damage D.C.P. Peacock1, C.W. Nixon1, A. Rotevatn1 & D.J. Sanderson2 1 Department of Earth Science, University of Bergen, Allégaten 41, 5007 Bergen, Norway 2 Engineering and the Environment, University of Southampton, Highfield, Southampton, SO17 1BJ, UK. …

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  • Christian Haug Eide

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

    Tana - a very old river: Linking an Early Triassic delta to antecedent topography The Fennoscandian Barents Sea Margin has been subject to little tectonic activity since the Carboniferous, and large portions have eluded significant Quaternary glacial erosion. Published fission …

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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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