Obukhov Formation
The Obukhov Formation is a geologic formation in Belarus and Ukraine that dates to the Late Eocene;[1] the Obukhov Formation is equivalent to the Prussian Formation of Russia. Rovno amber is found in this formation,[2] and 90% of amber collected from the Obukhov Formation is extracted illegally and the trade is controlled by armed organised crime groups.[2] Geological contextThe Late Eocene Rovno amber is hosted in the Obukhov Formation, and it underlies the Early Oligocene Mezhigorje Formation.[3][2] The formation is found along the northwestern margin of the Ukrainian Crystalline Shield[1] exposed in the Rivne region of Ukraine and across the border near Rechitsa in the Gomel Region of Belarus.[4] The granite basement rock was overlain by sandy to clayey deposits that were host to alluvial amber.[2] The two formations total between 2–7 m (6.6–23.0 ft) in thickness, both containing interbeds or mixtures of brown coals and carbonized vegetation. Both formations are sandy to clayey in texture, with the Obukhov Formation having more clayey glauconite-quartz plus sandy loess.[5] References
|
Portal di Ensiklopedia Dunia