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

Figure 5. The structure of the northern part of the Kharbei Block and the positions of the sites where
Samples 2127 and 2128 were collected for the isotopic and geochronology geochemical studies.
(1) the Orang zone, Ordovocoan sedimentary rocks, (2-7) the Kharbei Block complexes:
(2) schists and amphibolite, (3) gneiss and amphibolite,
(4) ultramafic rocks, (5) gabbroids, (6) diorite, (7) granite,
(8) faults and proposed faults.

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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