Publication Date:
2011-12-31
Description:
First finds of microfossils from the silicified microphytolitic carbonates of the Uluntui Formation in the southwestern Baikal region are described. They are represented by remains of the cyanobacterial community that formed microphytolites. These microfossils are accompanied by acritarchs probably belonging to green algae. The silicified microfossils are sufficiently well preserved despite complete and repeated recrystallization of host primary carbonate rocks. Main phases of secondary mineralization are related to hydrothermal-metasomatic processes, which were likely provoked by collisional events on the southern flank of the Siberian Craton in the Silurian. Content Type Journal Article Pages 89-97 DOI 10.1134/S0024490212010063 Authors A. M. Stanevich, Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences, ul. Lermontova 128, Irkutsk, 664033 Russia A. M. Mazukabzov, Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences, ul. Lermontova 128, Irkutsk, 664033 Russia T. A. Kornilova, Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences, ul. Lermontova 128, Irkutsk, 664033 Russia E. N. Maksimova, Irkutsk State Pedagogical University, ul. Nizhnyaya Naberezhnaya 6, Irkutsk, 664011 Russia Journal Lithology and Mineral Resources Online ISSN 1608-3229 Print ISSN 0024-4902 Journal Volume Volume 47 Journal Issue Volume 47, Number 1
Print ISSN:
0024-4902
Electronic ISSN:
1608-3229
Topics:
Geosciences
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