![]() RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 4, NO. 3, PAGES 171–186, doi:10.2205/2002ES000093, 2002
Geological complexes in the margin of the Siberian Craton as indicators of the evolution of a Neoproterozoic SupercontinentE. V. Sklyarov, D. P. Gladkochub, A. M. Mazukabzov, T. V. Donskaya, and A. M. Stanevich Institute of the Earth's Crust, Siberian Division, Russian Academy of Sciences,, RussiaAbstract
[1] This paper describes the Late Precambrian geologic
complexes from the southern margin of the Siberian Craton,
associated with the extension epochs. Analysis of the data
available suggests that there were two episodes of
intracontinental breakup, which resulted in the opening of the
ocean (1300-900 and 850-550 million years ago). The time
sequence of the "rift-related volcanic rocks and terrigenous
deposits
Received 22 May 2002; published 15 June 2002. Keywords: Siberian Craton, evolution of a Neoproterozoic Supercontinent, Late Precambrian geologic complexes. ![]() Citation: Sklyarov, E. V., D. P. Gladkochub, A. M. Mazukabzov, T. V. Donskaya, and A. M. Stanevich (2002), Geological complexes in the margin of the Siberian Craton as indicators of the evolution of a Neoproterozoic Supercontinent, Russ. J. Earth Sci., 4, No.3, 171-186, doi:10.2205/2002ES000093. Copyright 2002 by the Russian Journal of Earth Sciences Powered by TeXWeb (Win32, v.2.0). |