Publication
PECULIARITIES OF PEAT FORMATION IN UPPER NEO-PLEISTOCENE AND HOLOCENE OF THE CENTRAL PART OF THE WEST SIBERIAN PLAIN
(STEF92 Technology, 2019-06-20, Sergey Korkin)
Show more
Boggy deposits of the West Siberian Plain central are widespread covering min. 2/3 of the surface (excluding the floodplain) [1]. They are developed on all relief elements forming major wetlands, and their largest areas coincide with the I and II terraces raising above the floodplain of the Ob and its main feeders. Considering the Upper Pleistocene period, we will be concerned with MIS 3 deposits studied in the Kiryas section. In the beginning of MIS 2 (22-25 ths. years), the processes of deposition and peat accum...
Ecology and Environmental Protection2019