RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES4002, doi:10.2205/2007ES000224, 2008

Figure 11. Geotraverse of the Okhotsk Sea region
[Belousov and Udintsev, 1981;
Bikenina et al., 1987;
Bogdanov and Khain, 2000};
Piip and Rodnikov, 2004;
Rodnikov et. al., 1996, 2001;
Smirnov and Sugrobov, 1980;
Zlobin, 1987].
At the right top the geotraverse
position is shown. Below the distribution of measured values of the heat flow (mW m-2) is
shown along the profile. PZ - Paleozoic, MZ - Mesozoic, KZ - Cenozoic, K
2 - Upper
Cretaceous. 1 - location of earthquake hypocenters; 2 - faults; 3 - geological layers;
4 - isotherm, oC; 5 - boundaries of high conductivity layer; 6 - Moho discontinuity;
7 - seismic velocities, km s-1 ; 8 - water mass; 9 - volcanoes.

Citation: Rodnikov, A. G., N. A. Sergeyeva, L. P. Zabarinskaya, N. I. Filatova, V. B. Piip, and V. A. Rashidov (2008), The deep structure of active continental margins of the Far East (Russia), Russ. J. Earth Sci., 10, ES4002, doi:10.2205/2007ES000224.
Copyright 2008 by the Russian Journal of Earth Sciences
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