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

2005ES000187-fig02.html
Figure 2. Schematic geological profile across the South Tien Shan along the meridian of 68o30 prime (profile 1 in Figure 1): (1) the Low-Middle Paleozoic rocks, undifferentiated; (2) the Ordovician-Lower Silurian rocks, partially metamorphozed to green schists (Yagnob Schist); (3) the Devonian-Middle Carboniferous carbonate and siliceous-carbonate sediments; (4) the Lower-Middle Carboniferous volcanic rocks; (5) the Late Paleozoic, mostly flysch and molasse deposits; (6) the Mz-Kz platform-type terrigenous-carbonate and coarse-clastic molasse deposits; (7) granitoids of the Gissar batholith and of the axial zone of the Turkestan Ridge; (8) Permian acid volcanic rocks; (9) faults; (10) lithologic boundary; (11) names of the lithostructural zones: (AT) Afgan-Tajik, (SG) South-Gissar (including the Osmantala Zone), (CG) Central-Gissar, (KZ) Karakul-Zidda, (ZG) Zeravshan-Gissar (Yagnob), (ZT) Zeravshan-Turkestan, (Z) Zeravshan, (T) Turkestan, (NK) Nuratau-Kurganak, and (TA) Turkestan-Alai.

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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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