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

2007ES000223-fig17.html
Figure 17. Major units of the South Turkestan domain in the central 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 - neoautochthon.

RJES

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
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