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

2005ES000187-fig01.html
Figure 1. The schematic map of the main South Tien Shan structural elements: (1) the Mz-Kz sediments around the Tien Shan Mountains; (2) the Northern Tien Shan; (3) the Middle Tien Shan; (4-9) the Southern Tien Shan: (4) the outcropping rocks of the intrabasin volcanic (parautochthonous) ridges; (5) the outcropping allochthonous rocks of the intrabasin volcanic ridges; (6) the outcropping rocks of the relatively deep-sea troughs, volcanic high slopes, and shallow-sea bar slopes; (7) the outcrops of microcontinent sediments; (8) major collision sutures, listed in the northern direction: Karakul-Zidda, Zeravshan, Nuratau-Kurganak; (9) South Tien Shan structural features, undifferentiated; (10) Tarim, Suluterek, and South Gissar massifs; (11) Pamir structural features; (12) South Fergana ophiolite suture (Paleo-Turkestan ocean suture); (13) Talas-Fergana fault.

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
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