RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES1003, doi:10.2205/2006ES000194, 2006

2006ES000194-fig04.html
Figure 4. Results of the joint inversion of receiver functions, surface wave data, and traveltimes of converted waves from boundaries of the phase transition zone in the mantle. The top diagrams are the Vp and Vs velocity structures beneath the RUKSA array. The thin red lines bound the range of velocity variations in the inversion process. The middle curves are the observed (red) and synthetic (blue) receiver functions. The observed receiver function corresponds to curve C1+C3+C5 in Figure 2. The bottom plots show the observed (red circles) and calculated (blue line) phase velocities of Rayleigh waves. The traveltime of the converted Ps wave from the 410-km boundary is tps410 = 42.3  s (the ray parameter is 6.4 s/°.

RJES

Citation: Aleshin, I. M., G. L. Kosarev, O. Yu. Riznichenko, and I. A. Sanina (2006), Crustal velocity structure under the RUKSA seismic array (Karelia, Russia), Russ. J. Earth Sci., 8, ES1003, doi:10.2205/2006ES000194.

Copyright 2006 by the Russian Journal of Earth Sciences
Powered by TeXWeb (Win32, v.2.0).