Abstract
The results of studying the process of underthrusting in the Pacific plate under Kamchatka are presented, and the phenomena associated with this process are described. The seismic component of the velocity of the plate underthrust is estimated on the basis of (1) data from the CMT (Centroid Moment Tensor) catalog and (2) the sequence of the strongest Kamchatka earthquakes. A flat site with a strike azimuth of 217° and a dip angle of 25° located at depths of 30–70 km is assumed to be the interface between the plunging plate and Kamchatka. From CMT focal mechanisms, the underthrust velocity is estimated at V = 0.7 cm/yr for the southern zone (located south of Cape Shipunski) and at V = 1.1 cm/yr for the central zone (from Cape Shipunski to Cape Kronotski). From pairs of the strongest earthquakes that have occurred successively since 1737, the underthrust velocity for the southern zone is estimated at V = 6.6–7.1 cm/yr (from two pairs) and for the central zone, at V = 6.6 cm/yr. The creep portion of the underthrust amounts to 5–15% of the total velocity (the velocity of motion of the Pacific plate is 8 cm/yr).
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Original Russian Text © E.I. Gordeev, V.M. Pavlov, 2009, published in Fizika Zemli, 2009, No. 4, pp. 56–66.
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Gordeev, E.I., Pavlov, V.M. Subduction of the Pacific plate under Kamchatka: Seismic velocity of underthrust. Izv., Phys. Solid Earth 45, 326–337 (2009). https://doi.org/10.1134/S1069351309040053
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DOI: https://doi.org/10.1134/S1069351309040053