Abstract
A systematic comparative study of the reflectivity of the continental crust is undertaken ― made possible by the expanded data basis of deep seismic reflection profiles in Europe. The reflectivity is not at all the same but can change dramatically from one seismic line to the next. Different seismic reflectivity patterns ― independent of applied techniques ― are observed. Correlations between these seismic patterns and specific tectonic units have been found
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