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

2005ES000190-fig07.html
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 - pag 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.

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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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