Trubitsyn V.P.; Evseev M.N.; Trubitsyn A.P.(Федеральное государственное бюджетное учреждение науки Геофизический центр Российской академии наук, 2015)
The regularities of the global intraplate volcanism of the Earth are explained by the mantle plumes originating at the heads and margins of two piles of dense material of the hot and relatively heavy $D''$~layer at the ...
Trubitsyn V.P.; Evseev M.N.(Федеральное государственное бюджетное учреждение науки Геофизический центр Российской академии наук, 2016)
A mantle plume is a rising stream of vigorous thermal convection, which takes a mushroom-like shape and has a finite lifetime. When the plume approaches to the lithosphere the plume head first penetrates it. During the ...