Zobrazeno 1 - 10
of 30
pro vyhledávání: '"N. S. Balushkina"'
Autor:
O. V. Khotylev, Yu. A. Gatovsky, N. S. Balushkina, Yu. A. Kotochkova, N. I. Korobova, M. M. Fomina, E. V. Karpova, G. A. Kalmykov
Publikováno v:
Georesursy, Vol 23, Iss 2, Pp 120-131 (2024)
A different approach to the typing of the section of the Bazhenov Formation is presented – the identification of the reference section of the Bazhenov high-carbon formation (BHCF). Six packs were distinguished according to lithological and paleonto
Externí odkaz:
https://doaj.org/article/af9d9026bfbf4f1ebaa20855d7ef0cae
Autor:
M. M. Fomina, N. S. Balushkina, O. V. Khotylev, A. G. Kalmykov, G. A. Kalmykov, I. O. Reutskaya, S. A. Romanenko, M. S. Topchy, I. Ya. Bogatyreva, A. A. Alekhin
Publikováno v:
Georesursy, Vol 23, Iss 2, Pp 132-141 (2024)
The article presents the results of the Tutleim formation complex studies of core from 16 wells drilled on an area of 900 km2 near the Kamennaya crest of the Krasnoleninsky arch. The area is characterized by the variability of the structural plan, pr
Externí odkaz:
https://doaj.org/article/dda101be621a414c8e5290f584e14114
Autor:
E. V. Karpova, A. O. Khotylev, E. A. Manuilova, A. A. Mayorov, E. A. Krasnova, O. V. Khotylev, N. S. Balushkina, G. A. Kalmykov
Publikováno v:
Georesursy, Vol 23, Iss 2, Pp 142-151 (2024)
A model of the activity of hydrothermal-metasomatic systems confined to certain structural elements is proposed in the present article. The model is based on the analysis of a large volume of traditional studies: measurements of porosity coefficients
Externí odkaz:
https://doaj.org/article/9717b9a8a04f4b93b27f160e589319bb
Autor:
M. R. Latypova, O. V. Khotylev, N. S. Balushkina, A. G. Kalmykov, G. A. Kalmykov, L. F. Kopaevich, E. V. Karpova, V. V. Churkina
Publikováno v:
Moscow University Geology Bulletin. 77:48-60
Autor:
M. R. Latypova, O. V. Khotylev, N. S. Balushkina, A. G. Kalmykov, G. A. Kalmykov, L. F. Kopaevich, E. V. Karpova, V. V. Churkina
Publikováno v:
Moscow University Bulletin. Series 4. Geology. 1:49-60
As part of this work, various sedimentation environments were identified in the Middle-Late Jurassic (J2k–J3v1) on the territory of the Krasnoleninsky arch in Western Siberia. The heterogeneity of the seabed topography and the presence of islands f
Publikováno v:
Moscow University Bulletin. Series 4. Geology. 1:58-70
The regularities of changes in the lithological and geochemical composition of Bazhenov Formation (BF) rocks characterized by different degrees of organic matter transformation are determined. From МК1 2–МК2 (140–170 C–170–195 C), the fol
Autor:
G. A. Kalmykov, Inna O. Reutskaya, A. G. Kalmykov, Oleg V. Khotylev, N. S. Balushkina, Mariya S. Topchy, Stefaniya A. Romanenko, Alexander A. Alekhin, M. M. Fomina
Publikováno v:
Georesursy, Vol 23, Iss 2, Pp 132-141 (2021)
The article presents the results of the Tutleim formation complex studies of core from 16 wells drilled on an area of 900 km2 near the Kamennaya crest of the Krasnoleninsky arch. The area is characterized by the variability of the structural plan, pr
Autor:
E. A. Manuilova, Elizaveta A. Krasnova, N. S. Balushkina, Evgenia V. Karpova, Aleksandr A. Mayorov, Oleg V. Khotylev, Aleksey O. Khotylev, G. A. Kalmykov
Publikováno v:
Georesursy, Vol 23, Iss 2, Pp 142-151 (2021)
A model of the activity of hydrothermal-metasomatic systems confined to certain structural elements is proposed in the present article. The model is based on the analysis of a large volume of traditional studies: measurements of porosity coefficients
Autor:
N. I. Korobova, Oleg V. Khotylev, Yulia A. Kotochkova, Yury A. Gatovsky, Evgenia V. Karpova, N. S. Balushkina, M. M. Fomina, G. A. Kalmykov
Publikováno v:
Georesursy, Vol 23, Iss 2, Pp 120-131 (2021)
A different approach to the typing of the section of the Bazhenov Formation is presented – the identification of the reference section of the Bazhenov high-carbon formation (BHCF). Six packs were distinguished according to lithological and paleonto
Publikováno v:
Moscow University Geology Bulletin. 76:163-175
The regularities were determined for changes in the lithological and geochemical composition of rocks of the Bazhenov Formation (BF) characterized by various degrees of transformation of organic matter (OM). From the M $${\text{K}}_{2}^{1}$$ to MK2 s