• Evolution and structure of the Upper Rhine Graben — quantitative insights from numerical modelling approaches 

      Schwarz, Michael (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
      The Upper Rhine Graben forms the major segment of the Cenozoic Rift system of Western Europe. Although the rift was the target of many seismic and geological investigations, the style of lithospheric extension below the ...
    • Influence of viscosity on growth of high pressure phases in computer experiments 

      Sachau, Till; Koehn, Daniel (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
      The general aim of the project is the examination of microstructures that develop under HP conditions in computer experiments. Starting point is an interest in the dynamics of HP phase transitions, as for instance the ...
    • Kinematic 3D Retro-Deformation of Fault Blocks Picked from 3D Seismics 

      Tanner, David C.ORCIDiD; Lohr, Tina; Krawczyk, Charlotte M.ORCIDiD; Oncken, OnnoORCIDiD; Endres, Heike; Samiee, Ramin; Trappe, Henning; Kukla, Peter A.ORCIDiD (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
      Movement on fault planes causes a large amount of smaller-scale deformation, ductile or brittle, in the area surrounding the fault. Much of this deformation is below the resolution of reflection seismics (i.e. sub-seismic, ...
    • Structural investigation and strain analysis of a polyphase flower structure in the Lower Saxony Basin, Germany 

      Wagner, Lars; Lohr, Tina; Tanner, David C.ORCIDiD; Krawczyk, Charlotte M.ORCIDiD; Oncken, OnnoORCIDiD (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
      The Lower Saxony Basin (LSB) is a part of the post-Variscan Central European Basin System. We used a 3-D reflection seismic dataset in the northern LSB, provided by RWE-DEA AG, Hamburg (c.f. Lohr et al. submitted) for our ...
    • Über die mechanischen Ursachen von parallelen Abschiebungen 

      Nagel, Thorsten; Buck, Roger (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
      Gruppen von parallel einfallenden Abschiebungen treten in der Natur sehr häufig und in unterschiedlichsten Dimensionen auf. Existierende, überwiegend experimentelle Arbeiten führen einheitliches Einfallen auf laterale ...