Zobrazeno 1 - 6
of 6
pro vyhledávání: '"G. G. Akhmanov"'
Publikováno v:
Georesursy, Vol 25, Iss 4, Pp 42-57 (2024)
Group and molecular compositions of organic matter from bottom sediments of the northern sector of the Barents Sea were analysed. The sites where bottom sediments contain organic matter of molecular composition similar to that of oil are identified.
Externí odkaz:
https://doaj.org/article/696b04dc416745bdbeb542119c5d188c
Autor:
O. N. Vidishcheva, G. G. Akhmanov, E. V. Kislitsyna, A. Mazzini, A. Yu. Mal’tseva, E. N. Poludetkina, E. A. Bakay, I. E. Man`ko, D. V. Korost, O. M. Khlystov
Publikováno v:
Georesursy, Vol 24, Iss 2, Pp 209-216 (2024)
The paper presents results of gas-geochemical studies of bottom sediments and petroleum potential assessment of Baikal Rift Basin. During the expeditions of the Class@Baikal project in 2014–2019, gases from the Lake Baikal bottom sediments were ana
Externí odkaz:
https://doaj.org/article/54bea17e0f0b490dbdf774de7fee22a3
Publikováno v:
Georesursy, Vol 24, Iss 2, Pp 60-74 (2024)
At present time several dozen hydrocarbon fields are known in the Vendian-Cambrian complex of the Lena-Tunguska basin, which clearly does not exhaust its potential. The significant stratigraphic interval of the complex, its thickness (up to 3000 m),
Externí odkaz:
https://doaj.org/article/47da02da2d014697ad208801587f8245
Publikováno v:
Moscow University Bulletin. Series 4. Geology. 1:39-53
The paper presents the pore waters composition’s experimental results in the northeastern part of the Barents Sea. The pore water contains Cl–, Na+, SO4 2– and Mg2+ as dominant components and is quite similar to the Barents Seawater composition
Publikováno v:
Moscow University Geology Bulletin. 76:624-638
Autor:
A. K. Khudoley, S. V. Frolov, G. G. Akhmanov, E. A. Bakay, S. S. Drachev, A. Yu Egorov, V. B. Ershova, N. I. Korobova, N. S. Shevchuk, M. A. Rogov
Publikováno v:
Geological Society, London, Memoirs. 57
The Anabar–Lena Composite Tectono-Sedimentary Element (AL CTSE) is located in northern East Siberia extending for c. 700 km along the Laptev Sea coast between the Khatanga Bay and Lena River delta. The AL CTSE consists of rocks from the Mesoprotero