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Physical modeling of the formation conditions of marginal plateaux on the example of structures in the North Atlantic Ocean
Peculiarities of the formation of marginal plateaus in the early period of the opening of the North Atlantic Ocean are considered. The oceanic opening between Greenland and Europe (formation of the North Atlantic Ocean) began approx. 50–55 Mya after a long period of rifting, followed by the formation of the Aegir spreading ridge and the formation of the basin of the Norwegian Deep. Since that moment, the formation of a series of specific structures (marginal plateaus) began. The article considers conditions for their formation, using the physical modeling method. Three groups of structures were distinguished and typified according to the formation mechanism. A series of experiments was performed to each type of structures. Experimental results are compared with our proposed model for the formation and evolution of marginal plateaux.