The geochemical patterns of rocks of the Bazhenov and Abalak formations (Western Siberia)


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The composition of rocks of the Bazhenov and Abalak formations in Western Siberia is described. Correlations of the concentrations of the major and minor components in rocks with the concentrations of minor elements and organic material are shown. Study of the concentration of minor elements allows us to determine the conditions of sedimentation: redox potential, hydrogen sulfide contamination, and the source of sedimentary material. The results show that rocks of the Bazhenov Formation were formed under the conditions of low fluxes of clastic material, a reduced environment, and a periodically occurring hydrogen sulfide mode.

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A. Bychkov

Department of Geology

编辑信件的主要联系方式.
Email: andrewbychkov@rambler.ru
俄罗斯联邦, Moscow, 119991

G. Kalmykov

Department of Geology

Email: andrewbychkov@rambler.ru
俄罗斯联邦, Moscow, 119991

I. Bugaev

Department of Geology

Email: andrewbychkov@rambler.ru
俄罗斯联邦, Moscow, 119991

N. Balushkina

Department of Geology

Email: andrewbychkov@rambler.ru
俄罗斯联邦, Moscow, 119991

A. Kalmykov

Department of Geology

Email: andrewbychkov@rambler.ru
俄罗斯联邦, Moscow, 119991

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