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ON THE STRATIGRAPHIC SIGNIFICANCE OF THE LOW TERRACES OF THE SUZUN STRATA OF THE UPPER OB RIVER REGION. / Zolnikov, I. D.

в: Geology and Mineral Resources of Siberia, № 10s, 2021, стр. 7-17.

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

Harvard

Zolnikov, ID 2021, 'ON THE STRATIGRAPHIC SIGNIFICANCE OF THE LOW TERRACES OF THE SUZUN STRATA OF THE UPPER OB RIVER REGION', Geology and Mineral Resources of Siberia, № 10s, стр. 7-17. https://doi.org/10.20403/2078-0575-2021-10C-7-17

APA

Zolnikov, I. D. (2021). ON THE STRATIGRAPHIC SIGNIFICANCE OF THE LOW TERRACES OF THE SUZUN STRATA OF THE UPPER OB RIVER REGION. Geology and Mineral Resources of Siberia, (10s), 7-17. https://doi.org/10.20403/2078-0575-2021-10C-7-17

Vancouver

Zolnikov ID. ON THE STRATIGRAPHIC SIGNIFICANCE OF THE LOW TERRACES OF THE SUZUN STRATA OF THE UPPER OB RIVER REGION. Geology and Mineral Resources of Siberia. 2021;(10s):7-17. doi: 10.20403/2078-0575-2021-10C-7-17

Author

Zolnikov, I. D. / ON THE STRATIGRAPHIC SIGNIFICANCE OF THE LOW TERRACES OF THE SUZUN STRATA OF THE UPPER OB RIVER REGION. в: Geology and Mineral Resources of Siberia. 2021 ; № 10s. стр. 7-17.

BibTeX

@article{0228460a56d84fbab552b12d6d7f8c0b,
title = "ON THE STRATIGRAPHIC SIGNIFICANCE OF THE LOW TERRACES OF THE SUZUN STRATA OF THE UPPER OB RIVER REGION",
abstract = "Studies of the end of the 20th century showed that there are no sediments of the glacial-dammed lake-sea, as well as sediments of periglacial alluvium in sections of low terraces of the Upper Ob River region, known as the Suzun Strata. The lower stage of terraces is composed of alluvial sediments, and the upper one is represented by subaerial complex, which includes both deluvium and aeolian deposits. The height of areas varies significantly and is predetermined by thickness of the subaerial complex in each particular area. Сonsequently, the geomorphological principle does not work when differentiating the Suzun Strata into heterochronous geological bodies of accumulative terraces above the flood-plain.",
keywords = "Low terrace, Section, Stratigraphy, Suzun Strata, Upper Ob River Region",
author = "Zolnikov, {I. D.}",
note = "Publisher Copyright: {\textcopyright} И. Д. Зольников, 2021.",
year = "2021",
doi = "10.20403/2078-0575-2021-10C-7-17",
language = "русский",
pages = "7--17",
journal = "Геология и минерально-сырьевые ресурсы Сибири",
issn = "2078-0575",
publisher = "Федеральное государственное унитарное предприятие Сибирский научно-исследовательский институт геологии, геофизики и минерального сырья",
number = "10s",

}

RIS

TY - JOUR

T1 - ON THE STRATIGRAPHIC SIGNIFICANCE OF THE LOW TERRACES OF THE SUZUN STRATA OF THE UPPER OB RIVER REGION

AU - Zolnikov, I. D.

N1 - Publisher Copyright: © И. Д. Зольников, 2021.

PY - 2021

Y1 - 2021

N2 - Studies of the end of the 20th century showed that there are no sediments of the glacial-dammed lake-sea, as well as sediments of periglacial alluvium in sections of low terraces of the Upper Ob River region, known as the Suzun Strata. The lower stage of terraces is composed of alluvial sediments, and the upper one is represented by subaerial complex, which includes both deluvium and aeolian deposits. The height of areas varies significantly and is predetermined by thickness of the subaerial complex in each particular area. Сonsequently, the geomorphological principle does not work when differentiating the Suzun Strata into heterochronous geological bodies of accumulative terraces above the flood-plain.

AB - Studies of the end of the 20th century showed that there are no sediments of the glacial-dammed lake-sea, as well as sediments of periglacial alluvium in sections of low terraces of the Upper Ob River region, known as the Suzun Strata. The lower stage of terraces is composed of alluvial sediments, and the upper one is represented by subaerial complex, which includes both deluvium and aeolian deposits. The height of areas varies significantly and is predetermined by thickness of the subaerial complex in each particular area. Сonsequently, the geomorphological principle does not work when differentiating the Suzun Strata into heterochronous geological bodies of accumulative terraces above the flood-plain.

KW - Low terrace

KW - Section

KW - Stratigraphy

KW - Suzun Strata

KW - Upper Ob River Region

UR - http://www.scopus.com/inward/record.url?scp=85123209506&partnerID=8YFLogxK

U2 - 10.20403/2078-0575-2021-10C-7-17

DO - 10.20403/2078-0575-2021-10C-7-17

M3 - статья

AN - SCOPUS:85123209506

SP - 7

EP - 17

JO - Геология и минерально-сырьевые ресурсы Сибири

JF - Геология и минерально-сырьевые ресурсы Сибири

SN - 2078-0575

IS - 10s

ER -

ID: 35395042