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

2005ES000187-fig11.html
Figure 11. Geological profiles for the map shown in Figure 10: (1) modern tectono-gravitational mixtite; (2) Oligocene-Neogene red sandstone, gravelstone, and conglomerate; (3) Upper Cretaceous-Paleogene marl, claystone, sandstone, gypsum, and limestone; (4) Upper Cretaceous sandstone and claystone; (5) Jurassic conglomerate and sandstone; (6) Late Paleozoic flysch; (7) Lower-Middle Carboniferous chert and limestone; (8) Middle Devonian-Early Carboniferous sandstone and shale; (9) Middle Devonian-Early Carboniferous chert and limestone; (10) same as (9) in greenschist facies; (11) Late Ludlovian limestone; (12) Early Ludlovian limestone and dolomite; (13) Lower Silurian terrigenous rocks and greenschists; (14) faults; (15) boundaries of lithostructural zones; (16) pre-Mesozoic peneplane surface.

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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