Stratigraphy and Sedimentogenesis of the Clinoform Upper Jurassic of the Anabar–Lena Sedimentary Basin (Arctic Siberia, Laptev Sea Coast)

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Stratigraphy and Sedimentogenesis of the Clinoform Upper Jurassic of the Anabar–Lena Sedimentary Basin (Arctic Siberia, Laptev Sea Coast). / Devyatov, V. P.; Nikitenko, B. L.

в: Russian Geology and Geophysics, Том 64, № 11, 11.2023, стр. 1347-1357.

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

BibTeX

@article{7806ac40893d438b8a8e42b5a68f1488,

title = "Stratigraphy and Sedimentogenesis of the Clinoform Upper Jurassic of the Anabar–Lena Sedimentary Basin (Arctic Siberia, Laptev Sea Coast)",

abstract = "New materials on the stratigraphy and structural features of the Bathonian–Neocomian sections of the Anabar–Lena basin are presented. In the territory adjacent to the Taimyr mountain-folded system, a clinoform-like structure of the Upper Jurassic strata has been revealed, which are characterized by high thickness compared to adjacent sections in the east of this region. The lectostratotype of the Chernokhrebetnaya Formation (uppermost Lower Oxfordian–lowermost Volgian) is proposed. The most complete and continuous stratigraphic section is compiled, its litho-and chronostratigraphic correlations are given comparing to the sections of adjacent territories characterized in detail by fossil assamblages. The evidences for a new lithostratigraphic division of the territory are provided, facies zoning of sediments is clarified, a thickness chart of the Upper Bathonian–Boreal Berriasian strata of the Khatanga–Olenek interfluve is proposed.",

keywords = "Anabar–Lena sedimentary basin, Upper Bathonian–Lower Cretaceous, bio-, litho-, seismostratigraphy, clinoform structure, correlation, thickness analysis",

author = "Devyatov, {V. P.} and Nikitenko, {B. L.}",

note = "The authors are sincerely grateful to V.A. Kashirtsev and V.V. Sapyanik for fruitful discussions and comments that contributed to the improvement of the manuscript. The research was carried out with the support of RSF projects: No. 22-17-00054, No. 19-17-00091-P and the scientific and methodological support of the FTS (FWZZ-2022-0005). Публикация для корректировки.",

year = "2023",

month = nov,

doi = "10.2113/RGG20234620",

language = "English",

volume = "64",

pages = "1347--1357",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier Science B.V.",

number = "11",

}

RIS

TY - JOUR

T1 - Stratigraphy and Sedimentogenesis of the Clinoform Upper Jurassic of the Anabar–Lena Sedimentary Basin (Arctic Siberia, Laptev Sea Coast)

AU - Devyatov, V. P.

AU - Nikitenko, B. L.

N1 - The authors are sincerely grateful to V.A. Kashirtsev and V.V. Sapyanik for fruitful discussions and comments that contributed to the improvement of the manuscript. The research was carried out with the support of RSF projects: No. 22-17-00054, No. 19-17-00091-P and the scientific and methodological support of the FTS (FWZZ-2022-0005). Публикация для корректировки.

PY - 2023/11

Y1 - 2023/11

N2 - New materials on the stratigraphy and structural features of the Bathonian–Neocomian sections of the Anabar–Lena basin are presented. In the territory adjacent to the Taimyr mountain-folded system, a clinoform-like structure of the Upper Jurassic strata has been revealed, which are characterized by high thickness compared to adjacent sections in the east of this region. The lectostratotype of the Chernokhrebetnaya Formation (uppermost Lower Oxfordian–lowermost Volgian) is proposed. The most complete and continuous stratigraphic section is compiled, its litho-and chronostratigraphic correlations are given comparing to the sections of adjacent territories characterized in detail by fossil assamblages. The evidences for a new lithostratigraphic division of the territory are provided, facies zoning of sediments is clarified, a thickness chart of the Upper Bathonian–Boreal Berriasian strata of the Khatanga–Olenek interfluve is proposed.

AB - New materials on the stratigraphy and structural features of the Bathonian–Neocomian sections of the Anabar–Lena basin are presented. In the territory adjacent to the Taimyr mountain-folded system, a clinoform-like structure of the Upper Jurassic strata has been revealed, which are characterized by high thickness compared to adjacent sections in the east of this region. The lectostratotype of the Chernokhrebetnaya Formation (uppermost Lower Oxfordian–lowermost Volgian) is proposed. The most complete and continuous stratigraphic section is compiled, its litho-and chronostratigraphic correlations are given comparing to the sections of adjacent territories characterized in detail by fossil assamblages. The evidences for a new lithostratigraphic division of the territory are provided, facies zoning of sediments is clarified, a thickness chart of the Upper Bathonian–Boreal Berriasian strata of the Khatanga–Olenek interfluve is proposed.

KW - Anabar–Lena sedimentary basin

KW - Upper Bathonian–Lower Cretaceous

KW - bio-, litho-, seismostratigraphy

KW - clinoform structure

KW - correlation

KW - thickness analysis

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85176473003&origin=inward&txGid=cda64d95a0a7632cd57561e03ae1ca60

UR - https://www.mendeley.com/catalogue/d9f7d461-d76f-37c2-9c07-e6c80540d096/

U2 - 10.2113/RGG20234620

DO - 10.2113/RGG20234620

M3 - Article

VL - 64

SP - 1347

EP - 1357

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 11

ER -

ID: 59285551