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)

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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). / Rusakov, A.; Popov, A.; Pozdnyakova, A.

In: IOP Conference Series: Earth and Environmental Science , Vol. 368, No. 1, 012042, 28.11.2019.

Research output: Contribution to journal › Conference article › peer-review

BibTeX

@article{cc46b19d0abf49bda29600cfec4d3488,

title = "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)",

abstract = "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.",

author = "A. Rusakov and A. Popov and A. Pozdnyakova",

year = "2019",

month = nov,

day = "28",

doi = "10.1088/1755-1315/368/1/012042",

language = "English",

volume = "368",

journal = "IOP Conference Series: Earth and Environmental Science",

issn = "1755-1307",

publisher = "IOP Publishing Ltd.",

number = "1",

note = "International Conference on Key Concepts of Soil Physics: Development, Future Prospects and Current Applications 2019 ; Conference date: 27-05-2019 Through 31-05-2019",

}

RIS

TY - JOUR

T1 - 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)

AU - Rusakov, A.

AU - Popov, A.

AU - Pozdnyakova, A.

PY - 2019/11/28

Y1 - 2019/11/28

N2 - 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.

AB - 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.

UR - http://www.scopus.com/inward/record.url?scp=85077305537&partnerID=8YFLogxK

U2 - 10.1088/1755-1315/368/1/012042

DO - 10.1088/1755-1315/368/1/012042

M3 - Conference article

AN - SCOPUS:85077305537

VL - 368

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

SN - 1755-1307

IS - 1

M1 - 012042

T2 - International Conference on Key Concepts of Soil Physics: Development, Future Prospects and Current Applications 2019

Y2 - 27 May 2019 through 31 May 2019

ER -

ID: 51978027