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

Figure 8. Schematic geological map of the Merei R. and
Komissarovka R. basins (Merei suture zone). See Figure 4 for the
location of this area.
(1) Late Miocene-Quaternary;
(2) Late Eocene-Early Miocene; (3) Late Cretaceous-Paleocene
siltstone, argillite, siltstone interbedded by sandstones and marl
concretions; flyschoid interbedding of pelite, siltstone, and
sandstone; (4) Albian-Cenomanian siliceous argilaceous rock sequence
of tuffaceous siltstones and sandstones, tuffite, tuff, siliceous
siltstone, tuffaceous siltstone members of gradation structure;
(5) Lower Cretaceous tuffaceous-terrigenous rocks; (6) shale melange
(
1-2 ) with blocks and slabs of (a) jasper, (b) basalt,
(c) gabbro, and (d) serpentinite; (7) mylonite; (8) Ozerskii
Terrain; (9) overthrust and reversed faults: (a) pre-Late
Eocene, (b) Oligocene post-accretion; (10) shear and upthrust shear
faults; (11) faults of complex kinematics.

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
Powered by TeXWeb (Win32, v.2.0).