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

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.

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
Powered by TeXWeb (Win32, v.2.0).