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

Figure 7. Geological profiles across the Susunai Range.
(1) postmetamorphic rocks and their ages; (2) phyllite
and phyllite-like schists of the West Sakhalin Terrain
(K
1-2 -
11 ); (3-12) Susunai Terrain: (3-7) West Susunai
subterrain: (3-5) Krasnoselskaya metamorphic rock complexes (K
2 ):
(3) black schist, (4) green schist, (5) blue schist; (6, 7) Sokol
metamorphic rock series (J-K
1 ): (6) amphibolite,
(7) serpentinite; (8-12) East Susunai subterrain:
(8-11) metamorphic rock sequences: (8) Shuya (K
1-2 ), (9) Onega
(J-K
1 ), and (10) Annino (T-J), metabasalts: (a) tholeitic,
(b) subalkaline and alkaline; (11) metamorphic melange; (12) terrain
boundary.

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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