Central and Northern Europe has experienced several stages of geodynamic evolution leading to significant changes of topography in the past. Whereas the Caledonian and Variscan topographic evolution is caused by the collision of different plates at their borders the topographic and sedimentological evolution over the last 100 Myr in Central Europe occurs within the plate. Historically, fare field effects of the Alpine orogeny and the rotation of Spain are taken as the geodynamic cause for the change of the Central European Lithosphere. Nevertheless, the initial state and topography of the Central European Lithosphere at 100 Myr is important to understand the Post-100 Myr evolution. Significant exhumation, local subsidence and magmatic activities are key players during the last 100 Myr. Newly dated tectonic movements shed a new light on the multiple structural evolution during this time interval. As salt layers are important throughout the European lithosphere their influence on all processes have to be considered and understood. To unravel the geodynamic causes for the topographic evolution within the Central European plate various data sets have to be combined.
Therefore, the session seeks for contributions from Central to Northern Europe including the Alpine Orogeny by using tomography, seismic interpretations, thermochronology, structural interpretations, isotopic dating, sedimentology, salt deposits magmatic and metamorphic petrology and map interpretations. We would appreciate contributions describing the Early Mesozoic geodynamic evolution of Central Europe as well.
Guillocheau, Francois (1); Krob, Florian (1); Bunge, Hans-Peter (2); Francois Guillocheau, Francois (3)
1: Heidelberg University, Germany; 2: Ludwig-Maximilians-University Munich, Germany; 3: Université de Rennes 1, France