Upper mantle heterogeneity in the northern part of Eurasia

Details Upper mantle heterogeneity in the northern part of Eurasia Upper mantle heterogeneity in the northern part of Eurasia

Oct 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983pepi...33..180p&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 33, Issue 3, p. 180-193.

Physics

21

Scientific paper

A two dimensional velocity model of the upper mantle has been compiled from a long-range seismic profile crossing the West Siberian young plate and the old Siberian platform. It revealed considerable horizontal and vertical heterogeneity of the mantle. A sharp seismic boundary at a depth of 400 km outlines the high-velocity gradient transition zone, its base lying at a depth of 650 km. Several layers with different velocities, velocity gradients and wave attenuation are distinguished in the upper mantle. They likewise differ in their inner structure. For instance, the uppermost 50-70 km of the mantle are divided into blocks with velocities from 7.9-8.1 to 8.4-8.6 km s-1.
Comparison of the travel-time curves for the Siberian long-range profile with those compiled from seismological data for Europe distinguished large-scale upper mantle inhomogeneities of the Eurasian continent and allowed for the correlation of tectonic features and geophysical fields. The velocity heterogeneity of the uppermost 50-100 km of the mantle correlates with the platform age and heat flow, i.e., the young plates of Western Europe and Western Siberia have slightly lower velocities and higher heat flows than the ancient East European and Siberian platforms. At greater depths (150-250 km) the upper mantle velocities increase from the ocean to the inner parts of the continent. The structure of the transition zone differs significantly beneath Western Europe and the other parts of Eurasia. The sharp boundary at a depth of 400 km, traced throughout the whole continent as the boundary reflecting intensive waves, transforms beneath Western Europe into a gradient zone. This transition zone feature correlates with positions of the North Atlantic-west Europe geoid and heat-flow anomalies.

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