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

2005ES000187-fig13.html
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.

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).