The Upper Cretaceous deposits structure of Western Siberia
https://doi.org/10.31660/0445-0108-2021-5-51-68
Abstract
As the title implies the article presents the results of many years comprehensive research of the Western Siberian Upper Cretaceous stratigraphy (without Cenomanian). The volume of Upper Cretaceous formation, their biostratigraphic and lithological characteristics are discussed. Based on the analysis of new materials (lithological, biostratigraphic, well geophysics investigation data, magnetostratigraphic, seismostratigraphic), the regional correlation scheme of formations, members and beds has been refined. A new model of correlation schemes, a scheme of facies zoning, and reasonable changes in the nomenclature of the Upper Cretaceous formations are proposed. The Slavgorod and Ipatovo horizons have been replaced by a single Berezovo horizon. Specific properties description of the new suites, established at the first (Okhteurievo, Tagul, Bolshaya Laida, Nizhnaya Agapa), have been done.
About the Authors
V. A. Marinov
Tyumen Petroleum Scientific Center LLC; University of Tyumen
Russian Federation
Russian Federation
Vladimir A. Marinov, Candidate of Geology and Mineralogy, Expert
Tyumen
S. E. Agalakov
Tyumen Petroleum Scientific Center LLC
Russian Federation
Russian Federation
Sergey E. Agalakov, Senior Expert
Tyumen
T. V. Glukhov
Tyumen Petroleum Scientific Center LLC
Russian Federation
Russian Federation
Timofey V. Glukhov, Leading Specialist
Tyumen
A. I. Kudamanov
Tyumen Petroleum Scientific Center LLC
Russian Federation
Russian Federation
Alexander I. Kudamanov, Candidate of Geology and Mineralogy, Expert
Tyumen
M. Yu. Novoselova
Tyumen Petroleum Scientific Center LLC
Russian Federation
Russian Federation
Maya Yu. Novoselova, Chef Specialist
Tyumen
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Review
For citations:
Marinov V.A., Agalakov S.E., Glukhov T.V., Kudamanov A.I., Novoselova M.Yu. The Upper Cretaceous deposits structure of Western Siberia. Oil and Gas Studies. 2021;(5):51-68. (In Russ.) https://doi.org/10.31660/0445-0108-2021-5-51-68
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