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

Figure 3. The geodynamic evolution of the South Tien Shan in Ordovician-Late Carboniferous time
(Alai segment, see Profile 2 in Figure 1): (1) Kazakhstan-Kirgizian continental block; Turkestan paleooceanic
crust: (2) ultramafic layer, (3) gabbro-basalt layer, (4) sedimentary layer, (5) carbonate deposits (reefs),
(6) intrabasin volcanic underwater and island-arc ranges; (7) metamorphic volcanic rocks of intrabasin ridges;
(8) faults; (9) trend of tectonic rock flow.

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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