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

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 -
1 ), (7) Chaika rock sequence
(K
2 -
1 ), (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 (
1-2 ), (14) Vavai melange
(
22 ); (15) serpentinite; (16) melanocratic basement.

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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