LITHOLOGICAL AND MINERALOGICAL PECULIARITIES OF CARBONATE ROCKS IN THE UPPER TOURNAISIAN SUBSTAGE AT THE ALEKSEEVSKY OIL FIELD
https://doi.org/10.31660/0445-0108-2018-5-57-62
Abstract
At the present stage of the development of geological sciences more detailed lithological and petrographic studies become more important. Microscopic studies of core material in the Upper Taurus substage made it possible to isolate the lithotypes of carbonates characteristic of the investigated field. There are cloddy, clot-detrital, clay-detrital, and foraminifera-clotting lithotypes.The collectors are only limestones lumpy and clotty-detritus of the isolated structural-genetic differences. The study of the core material of the Upper Taurus substage of the Alekseevsky oil field allowed to conclude that the Kizel and Cherepets horizons are separate development objects.
Keywords
литотипы,
карбонаты,
кальцит,
детрит,
форамениферы,
lithotypes,
carbonates,
calcite,
detritus,
foraminifers
About the Authors
I. P. Zinatulluna
Kazan (Volga region) Federal University
Russian Federation
Russian Federation
L. B. Kadyrova
Almetyevsk State Oil Institute
Russian Federation
Russian Federation
References
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Review
For citations:
Zinatulluna I.P., Kadyrova L.B. LITHOLOGICAL AND MINERALOGICAL PECULIARITIES OF CARBONATE ROCKS IN THE UPPER TOURNAISIAN SUBSTAGE AT THE ALEKSEEVSKY OIL FIELD. Oil and Gas Studies. 2018;(5):57-62. (In Russ.) https://doi.org/10.31660/0445-0108-2018-5-57-62
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