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

Figure 13. Deformation of the pre-Mesozoic peneplain surface in the area of the Fan Mountains:
(1) Ordovician-Silurian metamorphic schists; (2) Late Silurian-Early Devonian limestone and marble;
(3) Middle Devonian-Early Carboniferous terrigenous siliceous-carbonate and flyschoid deposits and Late
Paleozoic flysch; (4) Mz-Kz conglomerate, sandstone, gypsum, claystone, limestone, and coal;
(5) Central Gissar Batholith granitoids; (6) faults; (7) the zone of high schistosity and mylonitization;
(8) structural and bedding lines; (9) pre-Mesozoic peneplain.

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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