Mz. Glukhovsky et Vm. Moralev, THE HOT BELT OF THE EARLY EARTH AND PRESE NT-DAY MANTLE GEODYNAMICS BASED ON SEISMIC TOMOGRAPHY DATA, Geologia i geofizika, 39(1), 1998, pp. 3-10
Published results of the seismic tomography of the entire Earth's mant
le were used for calculating areas of propagation of slow P-wave anoma
lies corresponding to a relatively hot mantle. The calculation was car
ried out within latitudinal intervals of 10 degrees for 14 levels from
78.1 to 2900 km in depth. The results obtained show the predominance
(58-86%) of hot mantle fields within the subequatorial belt at a depth
below 1000 km. This hot belt is considered as a relic of the Early Pr
ecambrian plume-tectonic stage of the Earth's evolution.