RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES6002, doi:10.2205/2005ES000187, 2005

Figure 6. The structural position of the Karakul Zone (Mz-Kz depression) in the Central
Tajik segment of the South Tien Shan: (1) the granitoids of the Central Gissar batholith;
(2) the Middle-Late Paleozoic terrigenous and carbonate rocks of the Gissar Zone; (3) the Late
Paleozoic (flysch) and Mz-Kz (terrigenous and carbonate) rocks of the Karakul Zone;
(4) the Middle Paleozoic carbonate rocks of the Dukdon Zone; (5) the Lower and Middle Paleozoic
rocks (metamorphic schist, shale, chert, and limestone) of the Zeravshan-Gissar Zone;
(6) the lines of the overthrust boundaries of the lithostructural zones;
(7) Boundary of structure formation zones.

Citation: Leonov, M. G. (2005), The Post-Oceanic Geodynamics of the South Tien Shan Region, Russ. J. Earth Sci., 7, ES6002, doi:10.2205/2005ES000187.
Copyright 2005 by the Russian Journal of Earth Sciences
Powered by TeXWeb (Win32, v.2.0).