In: Swiss Journal of Geosciences, 2008, vol. 101, no. 1, p. 139-183
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In: Earth and Planetary Science Letters, 1999, vol. 173, no. 3, p. 143-155
The western Alps form a geodynamically active mountain belt showing the typical features of an evolving orogenic wedge with its pro-wedge geometry to the NNW and its retro-wedge structures to the SSE. Renewed tectonic underplating of European continental crust occurred after the orogenic wedge underwent major dynamic disequilibrium following the break-off of the southward subducting slab of the...
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