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Neftyanaya Provintsiya 
No.4(28),2021, Part 1, Special issue
 

Specific aspects of scattered carbonaceous matter in Yu0 and Yu1 intervals of Em-Yogovsky field in Krasnoleninsky Arch

T.A. Ryazanova, R.R. Khasanov

DOI: https://doi.org/10.25689/NP.2021.4.35-54

PP.35-54

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Abstract

Micro-component organic matter composition has been analyzed, as well as its catagenetic maturity in the Upper Jurassic sediments of Em-Yogovsky field in the Krasnoleninsky Arch, West-Siberian petroleum basin.

A micro-component composition of concentrated (carbonaceous) organic matter in the Upper Jurassic sediments of Tutleimsky and Abalaksky formations has been studied for the first time using 304 samples from 11 Em-Yogovsky wells. Vitrinite reflectance has been measured and depositional environment has been specified. The most probable directions of hydrocarbon migration have been defined.

Key words:

carbon matter, micro-component composition, depositional environment, vitrinite reflectance, catagenetic maturity, coal grades, hydrocarbon generation

References

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Authors

T.A. Ryazanova, Ph.D., Geochemistry expert, Tyumen Petroleum Research Center

42, Maxim Gorky st, Tyumen, 625002, Russian Federation

E-mail: taryazanova@tnnc.rosneft.ru

 

R.R. Khasanov, Dr. Sc., Professor, Head of regional geology and mineral resources Department, Kazan Federal University

4/5, Kremlevskaya st., Kazan, 420008, Russian Federation

E-mail: Rinat.Khassanov@kpfu.ru

For citation:

T.A. Ryazanova, R.R. Khassanov Svoeobrazie rassejannogo ugleficirovannogo veshhestva plastov Ju0 i Ju1 Em-Egovskoj ploshhadi Krasnoleninskogo svoda [Specific aspects of scattered carbonaceous matter in Yu0 and Yu1 intervals of Em-Yogovsky field in Krasnoleninsky Arch]. Neftyanaya Provintsiya, No. 4(28), Part 1, Special issue, 2021. pp. 35-54. DOI https://doi.org/10.25689/NP.2021.4.35-54 (in Russian)

 
 
 

   © T.A. Ryazanova, R.R. Khassanov, 2021
       This is an open access article under the Creative Commons Attribution 4.0 License (https://creativecommons.org/licenses/by/4.0/)