Geochemical and mineral composition of bottom sediments of the last glaciosedimentation cycle from Lake Onega (NW, Russia)

Авторы

  • Malov, V.I. 1
  • Strahovenko, V.D. 1
  • Subetto, D.A. 2
  • Rybalko, A.V. 3
  • Belyaev, P.S. 3
  • Belkina, N.A. 4
  • Potakhin, M.S. 4
    • 1 V.S. Sobolev Institute of Geology and Mineralogy SB RAS, 3 Akademik Koptyug Prospect, Novosibirsk, 630090, Russia
    2 Herzen State Pedagogical University of Russia, 48 Moika Embankment, Saint-Petersburg, 191186, Russia
    3 A.P. Karpinsky Russian Geological Research Institute (VSEGEI), 74 Sredny Prospect, St. Petersburg, 199106, Russia
    4 Northern Water Problems Institute of the Karelian Research Centre RAS, 50 Alexander Nevsky Prospect, Petrozavodsk, 185030, Russia

DOI:

https://doi.org/10.31951/2658-3518-2022-A-4-1479

Ключевые слова:

Lake Onego, bottom sediments, Late Pleistocene, Holocene, geochemistry

Аннотация

The study of the geochemical and mineral composition of the bottom sediments of Lake Onega (the Petrozavodsk Bay) described fundamental differences between the chemical composition of sediments formed at the Holocene and Upper Pleistocene. It suggested the reason for mechanical to chemical type of weathering.

Загрузки

Опубликован

02.09.2022

Выпуск

2022: №4 (SI:Paleo2022)

Раздел

Статьи

Лицензия

Creative Commons License
Эта работа распространяется под международной лицензией Creative Commons Attribution-NonCommercial 4.0.