RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES5005, doi:10.2205/2006ES000201, 2006

Figure 1. Structure-tectonic scheme of the junction area of South Ural, Mugodzhary
and the Caspian Sea basin. Symbols: 1 - East European platform; 2 - Sol'-Iletskiy
subsided block; Ural folded belt: 3 - internides; 4-8 - externides: 4 - marginal
allochthons; 5 - Uraltauskiy anticlinorium (antiform); 6 - Kempirsayskiy anticlinorium
and Khabarninskiy synclinorium; 7 - Zilairskiy (in the north) and Kosisteksko-Aksuyskiy
(in the south) synclinoria; 8 - West Ural zone of linear folding and thrusts;
9 - Cis-Ural foredeep (figures in circles - 1), Aktyubinskiy (2) and Ostansukskiy (3)
troughs; Caspian Sea basin: 10 - carbonaceous platforms C2-P1;
11 - isohypse of subsalt Paleozoic complex
P II; The rest of symbols: 12 - Major Ural fault
(suture); 13 - Artinskian side scarp of Caspian Sea basin; 14 - tectonic dislocations;
15 - border of Khobdinskiy gravitational maximum; 16 - position of seismic profiles
obtained with the use of common depth point
[Kan, 1994].

Citation: Richter, Ya. A. (2006), A new concept of the junction nature of the Caspian Sea basin and Mugodzhar, Russ. J. Earth Sci., 8, ES5005, doi:10.2205/2006ES000201.
Copyright 2006 by the Russian Journal of Earth Sciences
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