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Publikováno v:
Geofizicheskiy Zhurnal; Том 36, № 2 (2014); 85-98
Геофизический журнал; Том 36, № 2 (2014); 85-98
Геофізичний журнал; Том 36, № 2 (2014); 85-98
Геофизический журнал; Том 36, № 2 (2014); 85-98
Геофізичний журнал; Том 36, № 2 (2014); 85-98
Within the framework of a three-dimensional P-velocity model of the mantle of the South-East Asia, the mantle velocity structure beneath Sumatra and its surroundings has been considered with the identification of possible premises in the deep structu