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

2005ES000188-fig02.html
Figure 2. Schematic map of the Enganepe Range structure: (1) undifferentiated Permian rocks; (2) undifferentiated Ordovician-Cambrian terrigenous-carbonate rocks; (3) in3 (?) to O 1 sandstones and conglomerates; (4) alkaline volcanic rocks; (5-9) pre-Ordovician rocks: (5) tuffaceous sedimentary rocks, (6) basalt and rhyolite, (7) a schists-olistostrome sequence with tectonic sheets and olistoliths, (8) undifferentiated tholeiitic basalt sequence, (9) a basalt-andesite-dacite complex, and (10) the position of the serpentinite melange area which was examined in detail in this study.

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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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