Abstract
The seismic and density models for the Earth’s crust of the central region of the Kuril Island arc are compared. The seismic data are based on the results of deep seismic soundings that were performed here in the 1980s. The density models were constructed by using marine and satellite gravimetric data obtained in recent years. Comparison of the seismic and density models reveals their overall consistency, with a few discrepancies. The possible sources of these discrepancies are discussed.
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