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

2005ES000187-fig03.html
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.

RJES

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).