Geocryological conditions of the Tokarikan and Guvilgra grabens (South Yakutia)
https://doi.org/10.31242/2618-9712-2023-28-2-261-274
Abstract
This article presents the results of geocryological studies of the Tokarikan and Guvilgra grabens of the Aldan Shield. Expedition research on the hard-to-rich region since 1996 has allowed us to determine the temperature regime, thickness, and nature of permafrost rock distribution and characterize its geocryological conditions for the first time. We have established that the lowest temperatures (up to –3.4 °С) are characteristic of peatmoss bog landscapes, whereas the highest (–0.5 °С) are for well-drained and watershed areas. The results of the measurements in deep wells, information on the process of drilling deep exploration wells, and the analysis of data on the thermophysical properties of rocks allowed us to estimate a permafrost thickness capacity that varied in the range of 40–260 m. The presented schematic permafrost and geological cross-sections and geocryological condition maps can be used to plan the industrial development of the territory.
Keywords
About the Authors
R. G. SYSOLYATINRussian Federation
SYSOLYATIN, Robert Gamletovich, Junior Researcher
ResearcherID: W-9244-2018, Scopus AuthorID: 1085009
Yakutsk
M. N. ZHELEZNYAK
Russian Federation
ZHELEZNYAK, Mikhail Nikolaevich, Corresponding member of the RAS, Dr. Sci. (Geol.-Mineral.), Director
ResearcherID: J-2544-2018, Scopus AuthorID: 70158
Yakutsk
References
1. Zheleznyak M.N. Geotemperature field and cryolithozone of South-East Siberian Platform. Novosibirsk: Nauka; 2005. (In Russ.)
2. Sysolyatin R.G., Zheleznyak M.N. Thermal regime of cryolithozone at Ytymdzha depression, Aldan shield. Earth’s Cryosphere. 2021;XXV(6):23–33.
3. Russia Coal Base. Volume VI. Cherepovsky V.F. (ed.). Moscow: Geoinformmark; 2004. (In Russ.)
4. Radkov A.V. et al. State Geological Map of the Russian Federation. Scale 1:1,000,000 (third generation). Aldan-Zabaikalskaya series. Sheet O-52 – Tommot. Explanatory note. St. Petersburg: Cartographic Factory of VSEGEI; 2016. (In Russ.)
5. Eastern Siberia. Komarov I.S. (ed.). Moscow: Moscow State University Press; 1978. (In Russ.)
6. Balobaev V.T. et al. Guidelines for the use of semiconductor thermistors for geocryological measurements. Yаkutsk: Permafrost Institute of the Siberian Branch of the USSR Academy of Sciences; 1985. (In Russ.)
7. Guglielmin M., Balks M. R., Adlam, L. S., Baio F. Permafrost Thermal Regime from Two 30-m Deep Boreholes in Southern Victoria Land, Antarctica. Permafrost and Periglacial Processes. 2011;22(2):129–139. https:// doi.org/10.1002/ppp.715
8. Geothermal features and frozen zone Suntar Hayata (on the example of the Nezhdaninsky deposit). Geoteplophysical research in Siberia. Pavlov A.V. (ed.). Novosibirsk: Nauka; 1978:129–142. (In Russ.)
9. Gavrilyev R.I. Method for determination of thermophysical properties of soils and rocks in quasistationary heating mode. Hydrothermal problems of frozen soils. Savvinov D.D. (ed.). Novosibirsk: Nauka; 1988:66–72. (In Russ.)
10. Lachenbruch A.H., Sass J.H., Marshall B.V., Moses T.H. Permafrost, heat flow, and the geothermal regime at Prudhoe Bay, Alaska. Journal of Geophysical Research. 1982;87(B11):9301–9316, https://doi.org/10.1029/JB087iB11p09301
11. Zheleznyak M.N. Some aspects of geocryological studies in the development of a rational variant of placement of engineering structures and the development of mineral deposits. The Extreme North: Problems of Ecology. Moscow: Resource-Info; 1999:57–59 (In Russ.)
12. Sysolyatin R. Characteristics of the Siberian coal basins permafrost: An example of Ytymdja depression. Science of The Total Environment. 2022;816:151494. https://doi.org/10.1016/j.scitotenv.2021.151494
13. Zhelinsky V.M. Mesozoic coal formation of South Yakutia. Novosibirsk: Nauka; 1980. (In Russ.)
14. Alekseyev V. R., Filosofov G.N. Orographic air temperature inversion in Eastern Siberia and its role in formation of permafrost rocks. Thermal and water regime of some Siberian regions. Leningrad: Nauka; 1970:102–107. (In Russ.)
15. Khrutsky S.F. On the history of formation of permafrost and ground ice in the Tipton-Gonam basin grabens. In: Kudryavtsev V.N. (ed.) Permafrost Investigations. Moscow: 1968;8:81–89. (In Russ.)
16. Geocryology of the USSR. Middle Siberia. Ershov E.D. (ed.). Moscow: Nedra, 1989. (In Russ.)
17. Baikal-Amur railway: geocryological map. Moscow: GUGK; 1979. (In Russ.)
18. Belokrylov I.D., Efimov A.I. Permafrost rocks of the zone of iron-ore and coal deposits of South Yakutia. Moscow: USSR Academy of Sciences Publishing House; 1960. (In Russ.)
19. Southern Yakutia. Permafrost, hydrogeolical, engineering and geological conditions of the Aldan mining industry region. Kudryavtsev V.A. (ed.). Moscow: Moscow University Press; 1975. (In Russ.).
20. Zheleznyak M.N. et al. Geocryological conditions of the Toka Depression. Proceedings of the First Conference of Russian Geocryologists, Moscow, June 3-5, 1996. Moscow: Publishing House of Moscow State University; 1996:522–528. (In Russ.)
Review
For citations:
SYSOLYATIN R.G., ZHELEZNYAK M.N. Geocryological conditions of the Tokarikan and Guvilgra grabens (South Yakutia). Arctic and Subarctic Natural Resources. 2023;28(2):261-274. (In Russ.) https://doi.org/10.31242/2618-9712-2023-28-2-261-274