A Model of the Accumulation of Radiolarite Layers in the Bazhenov Formation of West Siberia

被引:9
|
作者
Khotylev, O. V. [1 ]
Balushkina, N. A. [2 ]
Vishnevskaya, V. S. [3 ]
Korobova, N. I. [2 ]
Kalmykov, G. A. [2 ]
Roslyakova, A. S. [2 ]
机构
[1] Natl Intellectual Dev Fund, Moscow 119192, Russia
[2] Moscow MV Lomonosov State Univ, Dept Geol, Moscow 119234, Russia
[3] Russian Acad Sci, Geol Inst, Moscow 119017, Russia
基金
俄罗斯基础研究基金会;
关键词
Bazhenov Formation; radiolarite layers; radiolarians; currents; and relief; SEDIMENTS;
D O I
10.3103/S0145875219020054
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
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.
引用
收藏
页码:206 / 211
页数:6
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