Zobrazeno 1 - 10
of 84
pro vyhledávání: '"M. Spasennykh"'
Publikováno v:
SPE Reservoir Evaluation & Engineering. 26:64-74
Summary Organic matter-hosted pores are considered as the main type of porosity in organic-rich shales. At the same time, literature indicates the formation of pore space during pyrolysis of oil shales. However, controls, evolution, and types of orga
Autor:
Y. Popov, D. Ostrizhniy, E. Chekhonin, M. Spasennykh, R. Romushkevich, E. Moiseenko, S. Bogatov, S. Kirik
Publikováno v:
Rock Mechanics and Rock Engineering.
Publikováno v:
84th EAGE Annual Conference & Exhibition.
Akademický článek
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Akademický článek
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Publikováno v:
83rd EAGE Annual Conference & Exhibition.
Autor:
E. Chuvilin, B. Bukhanov, A. Yurchenko, D. Davletshina, N. Shakhova, E. Spivak, V. Rusakov, O. Dudarev, N. Khaustova, A. Tikhonova, O. Gustafsson, T. Tesi, J. Martens, M. Jakobsson, M. Spasennykh, I. Semiletov
Publikováno v:
Marine and petroleum geology. 2022. Vol. 138. P. 105550 (1-12)
Significant reserves of methane (CH4) are held in the Arctic shelf, but the release of CH4 to the overlying ocean and, subsequently, to the atmosphere has been believed to be restricted by impermeable subsea permafrost, which has sealed the upper sed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::02078771ecba19ab986c5fca789d738e
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996396
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000996396
Autor:
Z. Pichugin, E. Chekhonin, Y. Popov, M. Kalinina, I. Bayuk, E. Popov, M. Spasennykh, E. Savelev, R. Romushkevich, S. Rudakovskaya
Publikováno v:
Geothermics. 104:102456
Publikováno v:
Scopus-Elsevier
Summary A large number of studies have been published on the topic of acoustic wavefield modeling in anisotropic media. All of them are based on the choice of the suitable wave equation for numerical implementation. However, these wave equations are
Publikováno v:
30th International Meeting on Organic Geochemistry (IMOG 2021).
Summary The porosity of shales consists of mineral matrix voids and pores in organic matter. Since organic matter occupies up to 50% of source rock volume and most of the pores are connected, this type of porosity may considerably contribute to satur