In the study entitled «The effect of giant lateral collapses on magma pathways and the location of volcanism,» authored by F. Maccaferri, N. Richter and T. Walter, all working at GFZ, in section 2.1 (Physics of earthquakes and volcanoes), the propagation path of
magmatic intrusions underneath a volcanic edifice has been simulated by means of a mathematical model.
Tectonic -
magmatic (rift to drift) events on both the West and East Greenland margins are recorded by Paleocene and Early Eocene flood basalts, regional dike swarms, central
intrusions and sill complexes in Paleozoic - Mesozoic rift basins that have been exposed by Tertiary uplift.