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

2005ES000188-fig04.html
Figure 4. A diagram with a concordia for the isotope composition of the zircons collected from the gneiss (Sample 2127, grey ellipses) and gneissic granite (Sample 2128, black ellipses), collected from the Kharbei metamorphic rock complex.

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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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