RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES5002, doi:10.2205/2005ES000190, 2005

2005ES000190-fig05.html
Figure 5. Geological profiles across the Tonin-Aniva Peninsula. (1) neoautochthon, (2-5) Tonin-Aniva Terrain: (2) Evstafiev Formation (K 2 ), (3) Utesna rock sequence (K 1-2 ), (4) hard rock sequence (J-K 1 ), (5) Ostrovskii melange (K 1-2 ), (6-14) Ozerskii Terrain: (6) flysch and aleuropelite (K 2 - pag1 ), (7) Chaika rock sequence (K 2 - pag1 ), (8) Gorbusha rock sequence (K 1-2 ), (9) Kedrov rock sequence (J 3 -K 1 ), (10) Yunona rock sequence (T 2 -J), (11) Velikan rock sequence (P 2 -T 2 ), (12) jasper and basalt, (13) Okhotsk granodiorite ( pag1-2 ), (14) Vavai melange ( pag 22 ); (15) serpentinite; (16) melanocratic basement.

RJES

Citation: Zharov, A. E. (2005), South Sakhalin tectonics and geodynamics: A model for the Cretaceous-Paleogene accretion of the East Asian continental margin, Russ. J. Earth Sci., 7, ES5002, doi:10.2205/2005ES000190.

Copyright 2005 by the Russian Journal of Earth Sciences
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