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

Figure 10. The geological map of the Zeravshan basin area (the basins of the Rivat, Vashan, and
Madm Creeks): (1) Quaternary deposits; (2) Quaternary tectonic and gravitational mixtites;
(3) Oligocene-Neogene conglomerates, sandstone, and claystone; (4) Late Cretaceous-Paleogene marl,
claystone, sandstone, and gypsum (the vertical hatching shows the limestone and carbonate sandstone markers);
(5) Late Cretaceous conglomerates, sandstones, and claystones; (6) Liassic conglomerates and sandstones;
(7) Late Paleozoic flysch with limestone blocks and mesoliths (C
1-2 ); (8) Middle (Lower?)
Carboniferous limestone and chert; (9) unmetamorphozed rocks; (10) Middle Devonian-Lower Carboniferous
chert and terrigenous rocks in greenschist facies; (11) Upper Ludlovian limestone; (12) Lower Ludlovian
limestone and dolomite; (13-14) Llandoverian-Wenlockian rocks: (13) mainly limestone, (14) mainly
terrigenous rocks and green schists; (15) Lower Silurian sandy and shaly rocks of the Zeravshan-Turkestan Zone;
(16) olistolith composed of the rocks of the Kshtut-Urmeta Type; (17) the transgressive boundary between the
Mz-Kz rocks and the Paleozoic basement (pre-Mesozoic peneplane surface); (18) stratigraphic
boundary; (19) faults; (20) boundaries between the structure-formation zones; (21) dip and strike.

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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