| Authors |
Spector V.. candidate of geographical sciences, leading researcher, valentin_spektoг@mail. гиSpector V.. doctor of geological and mineralogical sciences, chief researcher, vspektoг@mail.гuBoeskorov G.. doctor of biological sciences, leading researcher, gboeskorov@mail.ruBelolyubsky I.. researcher, belolubsky@diamond .ysn.ruBakulina N.. head of the palynological group, г. Якутск, Россия |
| Bibliographic description |
Spector V., Spektor V., Boeskorov B., Belolyubsky I., Bakulina N. Periglacial alluvium of the Central Yakutiya plain according to the study of the bearing outcrop of Peschanaya Mountain // Transbaikal State University Journal, 2017, vol. 23, no. 5, pp. 45-59. |
| Annotation |
An aquatic genesis of the Late Pleistocene sediments (D’olkuminskaya suite), which had been considered as aeolian by many investigators, was proved in the southern part of the Central-Yakutian plain, in the bearing outcrop «Peschanaya Mountain» on the right bank of the Lena River. The sediments of the D’olkuminskaya suite were formed by catastrophic water flows of the NW-SE direction, which was opposite to the present-day direction of the Lena River course. The genesis is confirmed by granulometric, geochemical, and palynological investigations. The formation of sediments is, presumably, associated with a catastrophic flood in the end of Pleistocene |
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