![]() RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 5, NO. 5, PAGES 347–359, doi:10.2205/2003ES000125, 2003
Geologic complexes of the southern marginal part of the Siberian Craton as indicators of the Neoproterozoic supercontinent evolutionE. 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, Irkutsk, RussiaAbstract
[1] The aim of this paper is to discuss the Late Precambrian rock
complexes in the southern margin of the Siberian Craton, associated with the
extension. The analysis of the data available suggests two episodes of
intracontinental breakup which resulted in the opening of oceanic spaces
(1300-900 and 850-550 million years). The time sequence of "volcanogenic
terrigenous rocks of rifting origin
Received 16 June 2003; published 15 August 2003. Keywords: Siberian Craton, geologic complexes, Neoproterozoic supercontinent, intracontinental breakup, rifting. ![]() Citation: Sklyarov, E. V., D. P. Gladkochub, A. M. Mazukabzov, T. V. Donskaya, and A. M. Stanevich (2003), Geologic complexes of the southern marginal part of the Siberian Craton as indicators of the Neoproterozoic supercontinent evolution, Russ. J. Earth Sci., 5, No.5, 347-359, doi:10.2205/2003ES000125. Copyright 2003 by the Russian Journal of Earth Sciences Powered by TeXWeb (Win32, v.2.0). |