RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 10, ES1006, doi:10.2205/2007ES000223, 2008

Figure 10. Structure of major units of the South Turkestan domain in the western Tien Shan.
1 - Continental sediments; 2 - Conglomerates and breccias at the neoautochthon base;
3 - Shallow carbonate shelf sediments; 4 - Limestones and cherts accumulated in deeper
shelf; 5 - Volcanogenic sedimentary and volcanic rocks; 6 - Deep-water terrigenous and
siliceous-terrigenous sediments accumulated on continental slope and rise (flysch,
olistostromes, clayey rocks, etc.); 7 - Condensed deep-water siliceous and carbonate
siliceous sediments accumulated on continental slope and oceanic bottom; 8-9 - Oceanic
basalts, hyaloclastites, ignimbrites: 8 - slightly metamorphosed, 9 - metamorphosed;
10-11 - Age of overthrusting: 10 - most like (or most intense), 11 - less like
(or less intense). D-2, D-3, D-4 - deformation stages; neo-1, neo-2, neo-3 - neoautochthons.

Citation: Burtman, V. S. (2008), Nappes of the southern Tien Shan, Russ. J. Earth Sci., 10, ES1006, doi:10.2205/2007ES000223.
Copyright 2008 by the Russian Journal of Earth Sciences
Powered by TeXWeb (Win32, v.2.0).