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

2007ES000224-fig11.html
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.

RJES

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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