A Model of the Accumulation of Radiolarite Layers in the Bazhenov Formation of West Siberia
- Authors: Khotylev O.V.1, Balushkina N.A.2, Vishnevskaya V.S.3, Korobova N.I.2, Kalmykov G.A.2, Roslyakova A.S.2
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Affiliations:
- National Intellectual Development Fund
- Department of Geology, Moscow State University
- Geological Institute, Russian Academy of Sciences
- Issue: Vol 74, No 2 (2019)
- Pages: 206-211
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174940
- DOI: https://doi.org/10.3103/S0145875219020054
- ID: 174940
Cite item
Abstract
The Bazhenov Formation of West Siberia is one of the most important and promising high-carbon formations. Its peculiarity is a vast area and a high generation potential of constituent deposits. Another feature of this formation is the predominance of silicides, among which radiolarites that are often related to hydrocarbon inflows are the most interesting. However, the forecast procedure and their distribution nature are still disputable. Their formation model based on the interaction of plankton (radiolarians) and currents is proposed following the study of composition and textural features of the radiolarite layers in the clayey–siliceous rocks of the Bazhenov Formation.
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About the authors
O. V. Khotylev
National Intellectual Development Fund
Author for correspondence.
Email: hot63@mail.ru
Russian Federation, Moscow, 119192
N. A. Balushkina
Department of Geology, Moscow State University
Email: hot63@mail.ru
Russian Federation, Moscow, 119234
V. S. Vishnevskaya
Geological Institute, Russian Academy of Sciences
Email: hot63@mail.ru
Russian Federation, Moscow, 119017
N. I. Korobova
Department of Geology, Moscow State University
Email: hot63@mail.ru
Russian Federation, Moscow, 119234
G. A. Kalmykov
Department of Geology, Moscow State University
Email: hot63@mail.ru
Russian Federation, Moscow, 119234
A. S. Roslyakova
Department of Geology, Moscow State University
Email: hot63@mail.ru
Russian Federation, Moscow, 119234