Novel Mantle flow retrodictions reveal preferential material flow in the sublithospheric European mantle

Hans-Peter Bunge, Siavash Ghelichkhan & Jens Oeser
The Cenozoic tectonic evolution of Northern Europe involves a number of events that are difficult to reconcile with an intra-plate setting, including magmatic events and topographic changes that are located far from plate boundaries. It is entirely plausible to relate these events to sublithospheric processes in a vigorously convecting mantle. However, traditional mantle convection models are difficult to link to the spatiotemporal constraints provided by geologic archives, because their output invariably depends on the assumptions...
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