Reconstruction of Late Pleistocene sedimentation environment from data on catenary differentiation of soils and sediments along the northern slope of the Klin-Dmitrov Ridge (Russia)

A. Rusakov, A. Popov, A. Pozdnyakova

Результат исследований: Научные публикации в периодических изданияхстатья в журнале по материалам конференции

Аннотация

Based on analyzing the catenary sequence of soils and parent materials down the northern slope of the Klin-Dmitrov Ridge adjacent to the Upper Volga Lowland (formerly the periglacial zone of the Russian Plain), it was revealed that sediments including sandy loams, clay loams and clays, which constituted slope terraces at heights from 130 to 180 m a.s.l. and often accounted for lithic discontinuities in soil profiles, had glacio-lacustrine genesis, i.e., they had accumulated during the existence of a periglacial dammed lake at the final stages of the Late Pleistocene.

Язык оригиналаанглийский
Номер статьи012042
ЖурналIOP Conference Series: Earth and Environmental Science
Том368
Номер выпуска1
DOI
СостояниеОпубликовано - 28 ноя 2019
СобытиеInternational Conference on Key Concepts of Soil Physics: Development, Future Prospects and Current Applications 2019 - Moscow, Российская Федерация
Продолжительность: 27 мая 201931 мая 2019

Предметные области Scopus

  • Науки об окружающей среде (все)
  • Планетоведение и науки о земле (все)

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