Abstract
THE Alpine chain marks the collision zone between the European and African lithospheric plates. The Earth's crust below the Alps has been thickened by tectonic activity to form a 'root' of crustal material which extends to a depth of approximately 60 km. Here we present the initial results of three seismic reflection traverses across the Alps which show large-scale crustal indentations resulting from collision between continental plates, as well as the nappeforming style of deformation produced by compression of attenuated ocean crust. The data suggest that the gross structural deformation of the collision zone results from large-scale crustal indentations. The descending European crust is delaminated and deformed by wedges of the African crust protruding northwards below the Alps. The nappe-forming deformation seems to be restricted to the upper 10–20 km of the Penninic domain in the core of the Alps.
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Frei, W., Hertzmann, P., Lehner, P. et al. Geotraverses across the Swiss Alps. Nature 340, 544–548 (1989). https://doi.org/10.1038/340544a0
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DOI: https://doi.org/10.1038/340544a0
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