摘要
The Baikal Group is one of the most important stratigraphic units in the geology of East Siberia (Upper Riphean). This paper focuses on litological-facies features based on the analysis of organic remains (stromatolites, microphitolites and microfossils), in order to better precise the age and environmental deposit conditions of the Baikal Group. The results are used to draw a correlation between all the Precambrian of deposits of the South of East Siberia. The stratigraphy of the Baikal Group is then compared to the geodynamic evolution of this region, characterized by the break-up of the supercontinent Rodinia and subsequent opening of the Paleo-Asian Ocean. Stratigraphic analogs to the Baikal Group display in most areas deposits of various minerals (complex ores, phosphoresces, bauxites etc. have been dated of the same age), so the present study would also provides an economic interest.
The Baikal Group is one of the most important stratigraphic units in the geology of East Siberia （ Up- per Riphean）. This paper focuses on litological-facies features based on the analysis of organic remains （ strom- atolites, microphitolites and microfossils）, in order to better precise the age and environmental deposit condi- tions of the Baikal Group. The results are used to draw a correlation between all the Precambrian of deposits of the South of East Siberia. The stratigraphy of the Baikal Group is then compared to the geodynamic evolution of this region, characterized by the break-up of the supercontinent Rodinia and subsequent opening of the Paleo-A- sian Ocean. Stratigraphic analogs to the Baikal Group display in most areas deposits of various minerals （ com- plex ores, phosphoresces, bauxites etc. have been dated of the same age） , so the present study would also pro- vides an economic interest.
