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

Figure 2. Schematic map of the Enganepe Range structure: (1) undifferentiated Permian rocks;
(2) undifferentiated Ordovician-Cambrian terrigenous-carbonate rocks; (3)
3 (?) 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.

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).