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

Figure 7. The tectonic structure of the Karakul Basin: (1) Quaternary deposits;
(2-4) Cretaceous-Neogene deposits: (2) conglomerates and coarse sandstones,
(3) claystone, siltstone, sandstone, and gypsum, (4) limestone; (5) Middle-Late Carboniferous
sandstone and shale; (6) Middle-Late Carboniferous flysch; (7) Middle-Late Carboniferous flysch
transformed to "sedimentary" melange; (8) Lower-Middle Devonian limestone;
(9) outlier of the Lower-Middle Devonian limestone nappe; (10) Upper Silurian
limestone and dolomite; (11) Lower Silurian limestone, dolomite and shale; (12) tectonic breccia;
(13) Gissar Batholith granite; (14) structural line; (15) faults; (16) transgression contact.
The figures in circles are the numbers of the sections.

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
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