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

Figure 4. The geodynamic evolution of the Central Tajik segment of the South Tien Shan in Late
Silurian-Carboniferous time (Profile 1 in Figure 1). Shown in this figure is the morphostructural breaking of
the sea basin floor and the formation of the lock-joint subduction and ophiolite-devoid collision sutures.
(1) Mantle; (2) serpentinized ultrabasic rocks; (3) gabbro-basalt; (4) sedimentary rocks; (5) deposits
of intra-basin carbonate banks and platforms; (6) faults and tectonic break zones; (7) tectonic flow and rock
mass movement trends; (8) general compression of the region.

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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