Petrological and geochemical features of Middle Paleozoic basites in the Muna-Tyung interfluve region
https://doi.org/10.31242/2618-9712-2024-29-2-204-215
Abstract
The discovery of kimberlite pipes containing diamonds in the Viluy-Markha dyke belt led to a surge in interest in studying the products of Middle Paleozoic basic magmatism associated with these pipes in terms of their spatial and temporal characteristics. A distinct group of high-titanium rocks linked to diamond-bearing kimberlites was identified among the basic intrusions, serving as a key indicator for locating kimberlite pipes. This discovery prompted further research on basites and potential areas, such as the northeastern region of the dyke belt within the Muno-Tunga interfluve region, where alluvial diamonds have been found but their original sources remain unidentified. The presence ofdiamond varieties typical of kimberlites with high diamond concentrations in the placer diamonds of this area suggests the possibility of a new kimberlite field. The study of Middle Paleozoic basites in the Muno-Tunga interfluve region revealed high-titanium basites with similar petrochemical characteristics to those associated with diamond-bearing kimberlites. These basites are situated on the flanks of the dyke belt marked by compensating compression, making them a promising indicator for kimberlite prospecting. This study has demonstrated that areas with preferential compression are highly prospective for identifying primary diamond deposits.
About the Authors
A. G. KopylovaRussian Federation
Kopylova Albina Georgievna, Researcher
Yakutsk
S. S. Gogoleva
Russian Federation
Gogoleva Sargylana Semenovna, Leading Engineer
Yakutsk
References
1. Gayduk V.V. Vilyui Middle Paleozoic rift system. Yakutsk: YaSC SB USSR; 1988. 128 p. (In Russ.)
2. Polyansky O.P., Prokopiev A.V., Koroleva O.V., et al. Temporal correlation between the formation of dyke swarms and crustal extension in the middle Palaeozoic Vilyui rift basin, Siberian platform. Lithos. 2017;282- 283:45–64. https://doi.org/10.1016/j.lithos.2017.02.020
3. Tomshin M.D., Kopylova A.G., Konstantinov K.M., Gogoleva S.S. Basites of the Vilyui paleorift: Geochemistry and sequence of intrusive events. Russian Geology and Geophysics. 2018;59(10):1204–1216. https://doi.org/10.1016/j.rgg.2018.09.002
4. Tomshin M.D., Fomin A.S., Kornilova V.P., et al. Features of magmatic formations of the Nakyn kimberlite field of the Yakut province. Russian Geology and Geophysics. 1998;39(2):1693–1703. (In Russ.)
5. Mashchak M.S., Naumov M.V., Leukhin V.I., et al. Middle Paleozoic basic magmatism in the Nakyn Kimberlite Area (the Markha-Tjung interfluve). Regional Geology and Metallogeny. 2004;(20):122–138. (In Russ.)
6. Kiselev A.I., Ivanov A.V., Egorov K.N., Yarmolyuk V.V. Middle paleozoic basaltic and kimberlitic magmatism in the northwestern shoulder of the Vilyui rift, Siberia: Relations in space and time. Russian Geology and Geophysics. 2014;55(2):144–152.
7. Tomshin M.D., Zaitsev A.I., Zemnukhov A.L., Kopylova A.G. Character of basite formation in Nakyn kimberlite field, Yakutia. Otechestvennaya geologiya. 2004;(5): 39–43. (In Russ.)
8. Kopylova A.G., Zemnukhov A.L., Tomshin M.D. Petrochemical features of alkaline mafic rocks of the Nakyn kimberlite field. Otechestvennaya geologiya. 2005;(5): 65–73. (In Russ.)
9. Zemnukhov A.L., Zaitsev A.I., Kopylova A.G., et al. Basic magmatism of Khanna-Nakyn interfluve. In: Zinchuk N.N. (ed.). Geology of diamond – the present and the future. Voronezh: VGU; 2005, pp. 482–494. (In Russ.)
10. Tomshin М. D., Gogoleva S. S. High-titanium dolerites as a new criterion for kimberlite prospecting. Arctic and Subarctic Natural Resources. 2022;27(4):499–513. (In Russ.). https://doi.org/10.31242/2618-9712-2022-27-4-499-513
11. Kopylova A.G., Tomshin M.D. Maphic magmatism in the Middle Salakut Region. Nauka i obrazovaniye. 2008;52(4):27–33. (In Russ.)
12. Grakhanov S.A., Shatalov V.I., Shtyrov V.A., et al. Diamond placers of Russia. Novosibirsk: Geo; 2007. 454 p. (In Russ.)
13. Zinchuk N.N., Koptil’ V.I. Typomorphism of the Siberian platform diamonds. Moscow: Nedra; 2003. 603 p. (In Russ.)
14. Zintchouk N.N., Koptil’ V.I. Specific features of diamonds from the Siberian platform’s placers (in connection with forecasting problem of their primary sources). In: Geology of diamond – the present and the future. Voronezh: VGU; 2005, pp.1020–1050. (In Russ.)
15. Protsenko E.V. Gorev N.I. Prospects for the primary diamond content of the northeastern flank of the Vilyuisko-Markhinskaya mineragenic zone. In: Geology and mineral resources of the North-East of Russia: Proceedings of the 9th All-Russian scientific and practical conference: in 2 volumes, Yakutsk, 10– April 12, 2019. Volume 1. Yakutsk: NEFU Publishing House; 2019, pp. 160–165. (In Russ.)
16. Kalinin A.I., Zemnukhov A.L. Tectonic confirmation of the lateral zoning of the northeastern part of the VilyuiMarkhinsky dike belt. In: Problems of geology and subsoil development: proceedings of the 24th International Symposium named after Academician M.A. Usov students and young scientists, dedicated to the 75th anniversary of Victory in the Great Patriotic War, Tomsk, April 06–10, 2020. Tomsk: National Research Tomsk Polytechnic University. 2002, pp. 121–122. (In Russ.)
17. Sun S.-S., McDonough W.F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Saunders A.D., Norry M.J. (eds.). Magmatism in ocean basins. Geological Society. Special Publications. 1989;(42), pp. 313–345.
18. Gogoleva S.S., Kopylova A.G. Petrological and geochemical characteristics of the basites of the Tenkelyakh area. Arctic and Subarctic Natural Resources. 2019;24(1): 33–43. (In Russ.). https://doi.org/10.31242/2618-9712-2019-24-1-33-42
19. Bogatikov O.A., Gonshakova V.I., Efremova S.V., et al. Classification and nomenclature of igneous rocks. Moscow: Nedra; 1981. 160 p. (In Russ.)
20. Drake M.J., Weill D.F. Partition of Sr, Ba, Ca, Y, Eu+2, Eu+3, and other REE between plagioclase feldspar and magmatic liquid: an experimental study. Geochimica et Cosmochimica. Acta. 1975;39(5):689–712. https://doi.org/10.1016/0016-7037(75)90011-3
21. Oleynikov B.V., Tomshin M.D., Kopylova A.G., Rikhvanov L.P. Petrologo-geokhimicheskiye cherty lateral’noy zonal’nosti bazitov srednepaleozoyskikh paleoriftov Sibirskoy platformy. Otechestvennaya geologiya. 1997;(9):3–7. (In Russ.)
22. Wang K., Plank T., Walker J.D., Smith E.L. A mantle melting profile across the Basin and Range, SW USA. Journal of Geophysical Research: Solid Earth. 2002; 107(B1). https://doi.org/10.1029/2001JB000209.
23. Oleynikov B.V., Savvinov V.T Spatiotemporal evolution of trap magmatism within the Vilyui-Markha and Zhigansk magma supply zones. In: Kovalsky V.V., Oleynikov B.V. (eds.). Igneous formations of the northeast of the Siberian platform: (geology, petrography, mineralogy and geochemistry). Yakutsk; 1975, pp. 73–98. (In Russ.)
24. Kopylova A.G., Gogoleva S.S. Basites of TyungoMuna interfluece. In: Geology and mineral resources of the North-East of Russia: Proceedings of the 12th VNPK. Yakutsk: NEFU Publishing House; 2022, pp. 72–76. (In Russ.)
25. Khachatryan G.K., Zinchuk N.N., Koptil’ V.I. Structural defects in diamonds of the northeast of the Siberian platform and their typomorphic significance. In: Geology of diamond – the present and the future. Voronezh: VGU; 2005, pp.1607–1615. (In Russ.)
26. Ukhanov A.V., Nikol’skaya N.Ye., Galimov E.M., et al. Carbon isotope composition of diamonds from primary and alluvial deposits of the Yakut diamond-bearing province. In: Geology of diamond – the present and the future. Voronezh: VGU; 2005, pp. 1095–1111. (In Russ.)
Review
For citations:
Kopylova A.G., Gogoleva S.S. Petrological and geochemical features of Middle Paleozoic basites in the Muna-Tyung interfluve region. Arctic and Subarctic Natural Resources. 2024;29(2):204-215. (In Russ.) https://doi.org/10.31242/2618-9712-2024-29-2-204-215