The first data on the age of detrital zircons are given for Late Precambrian terrigenous rocks of the Baikal Group and Ushakovka Formation of the southern flank of the Siberian Craton. The ages obtained for 348 zircons cover the Paleoarchean to Late Ediacaran period, demonstrate the dynamics of change of sources of the clastic material in the sedimentation basin, and mark the changes of the Late Precambrian tectonic regimes. The age of the youngest group of detrital zircons extracted from the rocks of the Kachergat Formation allows us to restrict the upper age limit of accumulation of the rocks of the Baikal Group to the Late Ediacaran (Late Vendian). © 2013 Pleiades Publishing, Ltd.
Gladkochub, D. P., Nicoll, G., Stanevich, A. M., Mazukabzov, A. M., Sklyarov, E. V., Pisarevsky, S., Donskaya, T. V., & Tait, J. A. (2013). Age and Sources of Late Precambrian Sedimentary Sequences of the Southern Baikal Region: Results of the U–Pb LA-ICP-MS Dating of Detrital Zircons. Doklady Earth Sciences, 450(1), 494-498. https://doi.org/10.1134/S1028334X13050097