Palaeoproterozoic to Eoarchaean crustal growth in southern Siberia: a Nd-isotope synthesis

Gladkochub, Dmitry P. and Donskaya, Tatiana V. and Reddy, Steven M. and Poller, Ulrike and Bayanova, Tamara B. and Mazukabzov, Anatoliy M. and Dril, Sergei and Todt, Wolfgang and Pisarevsky, Sergei A. 2009. Palaeoproterozoic to Eoarchaean crustal growth in southern Siberia: a Nd-isotope synthesis, in Reddy, S.M., Mazumder, R., Evans, D.A.D, & Collins, A.S. (ed), Palaeoproterozoic supercontinents and global evolution. pp. 127-144. London, UK: Geological Society, London.

Source Title

Palaeoproterozoic supercontinents and global evolution

DOI

10.1144/SP323.6

ISBN

9781862392830

Faculty

Department of Applied Geology

Faculty of Science and Engineering

WA School of Mines

Remarks

Accepted for publication in Palaeoproterozoic supercontinents and global evolution as of 2009.

URI

http://hdl.handle.net/20.500.11937/5467

Collection

Curtin Research Publications

Abstract

Nd-isotope analyses from 114 rock samples are reported from the southern part of the Siberian craton to establish a first-order crustal formation scheme for the region. The Nd-isotopedata show considerable variability within and among different cratonic units. In many cases this variability reflects differing degrees of mixing between juvenile and older (up to Eoarchaean) crustal components. The fragments of Palaeoproterozoic juvenile crust within the studied segment of the Siberian craton margin have Nd-model ages of 2.0-2.3 Ga. Voluminous Palaeoproterozoicgranites ( 1.85 Ga) were intruded into cratonic fragments and suture zones. These granites mark the stabilization of the southern Siberian craton. The complexity in the Nd data indicatea long history of crustal development, extending from the Eoarchaean to the Palaeoproterozoiceras, which is interpreted to reflect the amalgamation of distinct Archaean crustal fragments, with differing histories, during Palaeoproterozoic accretion at 1.9-2.0 Ga and subsequent cratonic stabilization at 1.85 Ga. Such a model temporally coincides with important orogenic events on nearly every continent and suggests that the Siberian craton participated in the formation of a Palaeoproterozoic supercontinent at around 1.9 Ga.