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

Figure 15. Deep structure of the sedimentary trough in Tatar Strait. Above is a schematic location of the profile.
Geological age: PZ - Paleozoic, MZ - Mesozoic, K2 - Upper
Cretaceous, P - Paleogene, N - Neogene, Q - Quaternary. 1 - location of
earthquake hypocenters, 2 - faults, 3 - geological layers; 4 - isotherm, oC, 5 - water mass.

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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