Standard

The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain. / Rusakov, Alexey V.; Korkka, Mariya A.

в: Revista Mexicana de Ciencias Geologicas, Том 21, № 1, 01.12.2004, стр. 94-100.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Rusakov, AV & Korkka, MA 2004, 'The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain', Revista Mexicana de Ciencias Geologicas, Том. 21, № 1, стр. 94-100.

APA

Rusakov, A. V., & Korkka, M. A. (2004). The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain. Revista Mexicana de Ciencias Geologicas, 21(1), 94-100.

Vancouver

Rusakov AV, Korkka MA. The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain. Revista Mexicana de Ciencias Geologicas. 2004 Дек. 1;21(1):94-100.

Author

Rusakov, Alexey V. ; Korkka, Mariya A. / The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain. в: Revista Mexicana de Ciencias Geologicas. 2004 ; Том 21, № 1. стр. 94-100.

BibTeX

@article{e5480dc2e05b42a2aca64c9caaf68a2e,
title = "The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain",
abstract = "The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soil formed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (W{\"u}rmian) glaciation are described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene and corresponding to the marine isotope stage 3, is confined to the extraglacial zone of the Valday glaciation. The paleosol marks the northernmost area of existence of the Bryansk soil cover in Europe. It is shown that the Bryansk fossil soil can serve as a direct indicator of landscape and soil forming processes in the center of the Russian Plain.",
keywords = "Bryansk Soil, East-European Plain, Late Pleistocene, Moraine deposits, Paleosol, W{\"u}rmian glaciation",
author = "Rusakov, {Alexey V.} and Korkka, {Mariya A.}",
year = "2004",
month = dec,
day = "1",
language = "English",
volume = "21",
pages = "94--100",
journal = "Revista Mexicana de Ciencias Geologicas",
issn = "1026-8774",
publisher = "Universidad Nacional Autonoma de Mexico",
number = "1",

}

RIS

TY - JOUR

T1 - The Bryansk fossil soil of the extraglacial zone of the Valday glaciation as an indicator of landscape and soil forming processes in the center of the Russian Plain

AU - Rusakov, Alexey V.

AU - Korkka, Mariya A.

PY - 2004/12/1

Y1 - 2004/12/1

N2 - The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soil formed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (Würmian) glaciation are described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene and corresponding to the marine isotope stage 3, is confined to the extraglacial zone of the Valday glaciation. The paleosol marks the northernmost area of existence of the Bryansk soil cover in Europe. It is shown that the Bryansk fossil soil can serve as a direct indicator of landscape and soil forming processes in the center of the Russian Plain.

AB - The morphologic-analytical features of the Bryansk fossil soil classified as Umbric Gley Soil formed in moraine loams and overlain by Upper Pleistocene moraine of the Valday (Würmian) glaciation are described. This paleosol, formed during the Dunaevo Interstadial of the upper Pleistocene and corresponding to the marine isotope stage 3, is confined to the extraglacial zone of the Valday glaciation. The paleosol marks the northernmost area of existence of the Bryansk soil cover in Europe. It is shown that the Bryansk fossil soil can serve as a direct indicator of landscape and soil forming processes in the center of the Russian Plain.

KW - Bryansk Soil

KW - East-European Plain

KW - Late Pleistocene

KW - Moraine deposits

KW - Paleosol

KW - Würmian glaciation

UR - http://www.scopus.com/inward/record.url?scp=34848823601&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:34848823601

VL - 21

SP - 94

EP - 100

JO - Revista Mexicana de Ciencias Geologicas

JF - Revista Mexicana de Ciencias Geologicas

SN - 1026-8774

IS - 1

ER -

ID: 35467930