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Stratigraphy of the Lower and Middle Turonian (Upper Cretaceous) of the Yenisei (Left Bank) Part of West Siberia by Inoceramids and Foraminifers. / Marinov, V. A.; Agalakov, S. E.; Kosenko, I. N. et al.

In: Stratigraphy and Geological Correlation, Vol. 27, No. 4, 01.07.2019, p. 424-441.

Research output: Contribution to journal › Article › peer-review

Harvard

Marinov, VA, Agalakov, SE, Kosenko, IN, Urman, OS, Potapova, EA & Rozbaeva, GL 2019, 'Stratigraphy of the Lower and Middle Turonian (Upper Cretaceous) of the Yenisei (Left Bank) Part of West Siberia by Inoceramids and Foraminifers', Stratigraphy and Geological Correlation, vol. 27, no. 4, pp. 424-441. https://doi.org/10.1134/S0869593819040038

APA

Marinov, V. A., Agalakov, S. E., Kosenko, I. N., Urman, O. S., Potapova, E. A., & Rozbaeva, G. L. (2019). Stratigraphy of the Lower and Middle Turonian (Upper Cretaceous) of the Yenisei (Left Bank) Part of West Siberia by Inoceramids and Foraminifers. Stratigraphy and Geological Correlation, 27(4), 424-441. https://doi.org/10.1134/S0869593819040038

Vancouver

Marinov VA, Agalakov SE, Kosenko IN, Urman OS, Potapova EA, Rozbaeva GL. Stratigraphy of the Lower and Middle Turonian (Upper Cretaceous) of the Yenisei (Left Bank) Part of West Siberia by Inoceramids and Foraminifers. Stratigraphy and Geological Correlation. 2019 Jul 1;27(4):424-441. doi: 10.1134/S0869593819040038

Author

Marinov, V. A. ; Agalakov, S. E. ; Kosenko, I. N. et al. / Stratigraphy of the Lower and Middle Turonian (Upper Cretaceous) of the Yenisei (Left Bank) Part of West Siberia by Inoceramids and Foraminifers. In: Stratigraphy and Geological Correlation. 2019 ; Vol. 27, No. 4. pp. 424-441.

BibTeX

@article{76ae91b78b8a4ae7975a885437d7fe4c,
title = "Stratigraphy of the Lower and Middle Turonian (Upper Cretaceous) of the Yenisei (Left Bank) Part of West Siberia by Inoceramids and Foraminifers",
abstract = "Abstract—: The results of lithobiostratographic study of the lower part of the Late Cretaceous marine section are presented for the territory of the Bol{\textquoteright}shaya Kheta structural terrace on the left bank of the Yenisei River in its lower reaches (the upper parts of the Dolgan Formation, the Dorozhkovo Formation, and the lower parts of the Nason Formation; Turonian Stage). Eleven lithological members are traced in the territory and paleontologically characterized. The layers with fauna (inoceramids and foraminifers) are distinguished and compared with zonal Turonian subdivisions of West Siberia. It is found that the upper part of the Dolgan Formation belongs to the lower substage of the Turonian, Mytiloides labiatus Zone. The Dorozhkovo Formation in the region, which is close to its stratotypic locality, corresponds to the lower and middle Turonian.",
keywords = "biostratigraphy, foraminifers, inoceramids, Turonian, West Siberia",
author = "Marinov, {V. A.} and Agalakov, {S. E.} and Kosenko, {I. N.} and Urman, {O. S.} and Potapova, {E. A.} and Rozbaeva, {G. L.}",
year = "2019",
month = jul,
day = "1",
doi = "10.1134/S0869593819040038",
language = "English",
volume = "27",
pages = "424--441",
journal = "Stratigraphy and Geological Correlation",
issn = "0869-5938",
publisher = "PLEIADES PUBLISHING INC",
number = "4",

}

RIS

TY - JOUR

T1 - Stratigraphy of the Lower and Middle Turonian (Upper Cretaceous) of the Yenisei (Left Bank) Part of West Siberia by Inoceramids and Foraminifers

AU - Marinov, V. A.

AU - Agalakov, S. E.

AU - Kosenko, I. N.

AU - Urman, O. S.

AU - Potapova, E. A.

AU - Rozbaeva, G. L.

PY - 2019/7/1

Y1 - 2019/7/1

N2 - Abstract—: The results of lithobiostratographic study of the lower part of the Late Cretaceous marine section are presented for the territory of the Bol’shaya Kheta structural terrace on the left bank of the Yenisei River in its lower reaches (the upper parts of the Dolgan Formation, the Dorozhkovo Formation, and the lower parts of the Nason Formation; Turonian Stage). Eleven lithological members are traced in the territory and paleontologically characterized. The layers with fauna (inoceramids and foraminifers) are distinguished and compared with zonal Turonian subdivisions of West Siberia. It is found that the upper part of the Dolgan Formation belongs to the lower substage of the Turonian, Mytiloides labiatus Zone. The Dorozhkovo Formation in the region, which is close to its stratotypic locality, corresponds to the lower and middle Turonian.

AB - Abstract—: The results of lithobiostratographic study of the lower part of the Late Cretaceous marine section are presented for the territory of the Bol’shaya Kheta structural terrace on the left bank of the Yenisei River in its lower reaches (the upper parts of the Dolgan Formation, the Dorozhkovo Formation, and the lower parts of the Nason Formation; Turonian Stage). Eleven lithological members are traced in the territory and paleontologically characterized. The layers with fauna (inoceramids and foraminifers) are distinguished and compared with zonal Turonian subdivisions of West Siberia. It is found that the upper part of the Dolgan Formation belongs to the lower substage of the Turonian, Mytiloides labiatus Zone. The Dorozhkovo Formation in the region, which is close to its stratotypic locality, corresponds to the lower and middle Turonian.

KW - biostratigraphy

KW - foraminifers

KW - inoceramids

KW - Turonian

KW - West Siberia

UR - http://www.scopus.com/inward/record.url?scp=85070823707&partnerID=8YFLogxK

U2 - 10.1134/S0869593819040038

DO - 10.1134/S0869593819040038

M3 - Article

AN - SCOPUS:85070823707

VL - 27

SP - 424

EP - 441

JO - Stratigraphy and Geological Correlation

JF - Stratigraphy and Geological Correlation

SN - 0869-5938

IS - 4

ER -

ID: 21253656