RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 7, ES5003, doi:10.2205/2005ES000188, 2005

2005ES000188-fig01.html
Figure 1. Schematic tectonic map of the Polar Ural region after [Didenko et al., 2001] modified after [Shishkin, 2005]: (1) the autochthon of the Western Ural zone, composed of Riphean-Cambrian metamorphic rocks and the protoUral rocks of the East Ural zone; (2) the para-autochthon and allochthon of the West Ural Zone, composed of Paleozoic stratified rocks; (3-4) the Central Ural Zone: (3) the Orang subzone, composed of Paleozoic and Late Paleozoic stratified rocks; (4) the Kharbei subzone, preordovician rocks including Late Paleozoic stratified rocks; (5-9) the East Ural Zone: (5) the Marunkeu subzone, high-pressure metamorphic rocks; (6) the Khord-Yus-Delayus subzone composed mostly of metamorphic mafic rocks, (7) the Syumkeu-Payera (Voikar–Rai-Iz) subzone of the mafic-ultramafic rock belt; (8-9) the Minor-Ural subzone of Devonian and Carboniferous granites (8)and the volcanic rocks (9) associated with them. The protoUral rocks occur as the Enganepe (E) and Kharbei (Khb) complexes; the metabasic rocks have been classified as the Marunkeu (M), Khord-Yus (Kh), and Dzelayu (D) complexes; the mafic-ultramafic rocks have been classified as the massifs of the mafic-ultramafic rock belt known as the Syumkeu (S), Rai-Iz (R), and Voikar-Synya massifs.

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Citation: Khain, E. V., A. A. Fedotova, E. V. Bibikova, E. B. Salnikova, A. B. Kotov, K.-P. Burgat, V. P. Kovach, and D. N. Remizov (2005), The Neoproterozoic and Early Paleozoic geological history of the Ural-Kazakhstan margin of the Paleoasian Ocean using new isotopic and geochronological data obtained for the Polar Ural region, Russ. J. Earth Sci., 7, ES5003, doi:10.2205/2005ES000188.

Copyright 2005 by the Russian Journal of Earth Sciences
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