Abstract
The gravitational and magnetic fields of the eastern Aldan anteclise, within the area bounded by longitudes 126° and 138° E and latitudes 58° and 64° N, are analyzed; seismic data along the 3-DV Tommot‒Khandyga reference profile are also considered in order to identify structural features of the Early Precambrian consolidated crust and to assess the diamond potential of the territory. It is shown that the crystalline basement is divided by the Uchur crustal‒mantle fault into the Paleoproterozoic Aldan granulite–gneiss belt and the Archean Batomga granite–greenstone zone; the southern segments of these structures were studied within the Aldan–Stanovoy shield. The formation processes of the Aldan granulite–gneiss belt in the Paleoproterozoic contributed to thickening of its crust (to 50–52 km) compared to the Archean Batomga granite–greenstone region (42–45 km). The Khompu–Maya kimberlite field with the Tuymada pipe is confined to the Bestyakh block of the Batomga granite–greenstone zone. The main regional criteria for the diamond potential of the identified subprovince in the northeast Aldan anteclise include: (i) the presence of a lithospheric root up to 220 km thick, (ii) the granite–greenstone type of the Earth’s crust, and (iii) low heat flow values.
Similar content being viewed by others
REFERENCES
V. T. Balobaev, Geothermal Measurements in the Permafrost of Northern Asia (Nauka, Novosibirsk, 1991) [in Russian].
V. I. Vaganov, Yu. K. Golubev, and N. A. Prusakova, “The stage prospecting geological works for diamonds in the East European Platform,” in Geology of Diamond—Present and Future, Ed. by N. N. Zinchuk (Voronezh. Gos. Univ. Voronezh, 2005), pp. 1124–1136 [in Russian].
The 1 : 5 000 000 Geological Map of Russia and Adjacent Countries (within the Borders of the Former USSR), Ed. by R. I. Sokolov (Vseross. Nauchno-Issled. Geol. Inst., St. Petersburg, 1992) [in Russian].
E. Yu. Goshko, A. S. Efimov, and A. S. Sal’nikov, “The recent structure and the assumed history of formation of the crust in the south-eastern segment of the North Asian craton along Reference Profile 3-DV,” Geodynam. Tectonophys., No. 3, pp. 785–798, 2014.
E. Yu. Goshko, A. S. Sal’nikov, and A. V. Migurskii, “Frequency-dependent energy analysis of CDP seismic sections for geological interpretation,” Geofizika, No. 1, 32–39, 2011.
The 1 : 2 500 000 Gravimetric Map of the SSSR, Ed. by P. P. Stepanov and M. A. Yakushevich (VNII “Geofizika”, Moscow, 1990) [in Russian].
V. S. Grinenko, V. A. Kamaletdinov, Yu. L. Slastenov, and O. I. Shcherbakov, “Geological structure of Bolshoi Yakutsk,” in Regional Geology of Yakutia, Ed. by Yu. L. Slastenov (Yakutsk. Gos. Univ. Yakutsk, 1995), pp. 3–20 [in Russian].
G. S. Gusev, A. F. Petrov, and G. S. Fradkin, Structure and Evolution of the Earth’s Crust in Yakutia (Nauka, Moscow, 1985) [in Russian].
A. V. Egorkin, S. K. Zyuganov, N. A. Pavlenkova, and N. M. Chernyshev, “The results of exploring the structure of the lithosphere on the profiles in Siberia,” Geol. Geofiz., No. 5, 120–128, 1988.
A. S. Egorov, Deep Structure and Geodynamics of Lithosphere in North Eurasia with the Geological-Geophysical Modeling along Geotraverses in Russia as Example (Vseross. Nauchno-Issled. Geol. Inst., St. Petersburg, 2004) [in Russian].
The 1 : 1 000 000 Map of Anomalous Magnetic Field of Russia and Adjacent Water Areas, Ed. by T. P. Litvinova and Z. A. Makarova (Vseross. Nauchno-Issled. Geol. Inst., St. Petersburg, 1995) [in Russian].
S. N. Kashubin, O. V. Petrov, E. D. Mil’shtein, I. V. Kudryavtsev, E. A. Androsov, I. Yu. Vinokurov, O. A. Tarasova, and Yu. M. Erinchek, “Deep structure of the crust and upper mantle of Northeast Eurasia,” Regional. Geol. Metallogen., No. 76, 9–21, 2018.
A. V. Kotov, Doctoral Dissertation in Geology and Mineralogy (IGGD RAN, St. Petersburg, 2003).
A. V. Manakov, “Regional geophysical criteria of prediction of primary diamond potential,” in Geophysics of Yakutia into the XXI Century, Ed. by V. V. Stogny (Yakutsk. Gos. Univ., Yakutsk, 2001), pp. 158–168 [in Russian].
M. V. Mints, “Seismic images of the crust-mantle boundary as an expression of geodynamics of the Precambrian crust formation,” Geofiz. Issled. 17 (1), 65–82 (2016).
V. M. Mishnin, A. P. Andreev, K. A. Bekrenev, and Z. A. Altukhova, “A new geophysical approach to mineragenic zoning of Siberian Platform and prospect of the diamond-bearing potential of the Yakut buried uplift,” Litosfera, No. 5, 30–52, 2011.
V. M. Mishnin and V. S. Grinenko, “The Atlantic/Pacific divide: the main trend of commercial diamondiferous taxons large in linear extent,” in Geology of Diamond—Present and Future, Ed. by N. N. Zinchuk (Voronezh. Gos. Univ., Voronezh, 2005), pp. 132–149 [in Russian].
K. B. Mokshantsev, D. K. Gornshtein, and A. A. Gudkov, Deep structure of the Eastern Siberian Platform and Adjacent Folded Structures in the Verkhoyansk–Chukotka Region (Nauka, Moscow, 1968) [in Russian].
P. O. Polyansky, A. F. Emanov, A. S. Sal’nikov, and V. V. Zhabin, “Dynamic conversion of head waves on the central part of the 3-DV profile: Technique features and interpretation of time sections,” Geofiz. Issled. 19 (2), 5–33, 2018.
O. M. Rozen, “Siberian Craton: Tectonic zoning and evolutional stages,” Geotectonics 41 (3), 3–21, 2003.
O. M. Rozen, A. V. Manakov, and N. N. Zinchuk, Siberian Craton: Formation and Diamond Potential (Nauchn. Mir, Moscow, 2006).
D. I. Rudnitskaya, V. S. Starosel’tsev, and A. S. Sal’nikov, “The construction of the Earth’s crust macromodel applying the Reapak-technology along the 3-DV geotraverse (East Siberia,” Geofizika, No. 1, 19–26, 2013.
A. V. Sagir, “Character of development and metallogeny of the Sette Daban palaeorift,” Otech. Geol., No. 2, 17–23, 1997.
A. P. Smelov, E. A. Belousova, A. I. Zaitsev, O. B. Oleinikov, A. D. Pavlushin, and N. A. Oparin, “First data on composition and age of the buried basement of the Aldan anteclise (Siberian Platform): dating of xenogenic zircon from the Manchary kimberlite pipe,” Otech. Geol., No. 5, 68–72, 2013.
A. P. Smelov, V. D. Gabyshev, V. P. Kovach, and A. B. Kotov, “General structure of the basement of the eastern part of the Craton,” in Tectonics, Geodynamics, and Metallogeny of the Republic of Sakha (Yakutia), Ed. by L. M. Parfenov and M. I. Kuzmin (MAIK “Nauka/Interperiodika,” Moscow, 2001), pp. 108–112 [in Russian].
A. E. Sobolev, “Khandyga ring tectonomagmatic macrostructure,” Geol. Geofiz., No. 3, 33–39, 1985.
V. V. Stogny and G. A. Stogny, Tectonic Layering of the Aldan–Stanovoy Geoblock (Nauka, Novosibirsk, 1997) [in Russian].
G. A. Stogny and V. V. Stogny, Geophysical fields of the Eastern North Asian Craton (Sakhapoligrafizdat, Yakutsk, 2005) [in Russian].
G. A. Stogny and V. V. Stogny, “Regional lithospheric heterogeneities of North Asian Craton,” Geofizika, No. 6, 59–65, 2009.
G. A. Stogny and V. V. Stogny, “Regional criteria of prediction of kimberlite subprovince in the east of Siberian Platform based on interpretation of gravimagnetic data,” in Ore Genesis and Metallogeny of East Asia, Ed. by V. A. Trunilina (Yakutsk. Gos. Univ., Yakutsk, 2006), pp. 188–191 [in Russian].
V. D. Suvorov and Z. A. Kornilova, “Deep structure of the Aldan Shield on the basis of seismic data on close earthquakes,” Geol. Geofiz., No. 2, 86–93, 1985.
V. D. Suvorov and E. A. Mel’nik, “Seismic structure of the Earth’s crust in the junction zone of the Siberian Craton and the Verkhoyansk–Kolyma fold system,” Interekspo Geo-Sibir’ 4, 264–271, 2018.
Tectonics, Geodynamics, and Metallogeny of the Republic of Sakha (Yakutia), Ed. by L. M. Parfenov and M. I. Kuzmin (MAIK “Nauka/Interperiodika,” Moscow, 2001) [in Russian].
Tectonics, Deep Structure, Metallogeny in the Conjunction Zone between Central Asian and Pacific Belts, Ed. by L. P. Karsakov, Chunjing Zhao, Yu. F. Malyshev, and M. V. Goroshko (Vladivostok–Khabarovsk, Dalnevost. Otd. Ross. Akad. Nauk, 2005) [in Russian].
The 1 : 1 500 000 Tectonic Map of the Yakutsk ASSR and Adjacent Areas, Ed. by K. B. Mokshantsev (GUGK, Moscow, 1976) [in Russian].
A. D. Khar’kiv, N. N. Zinchuk, and A. I. Kryuchkov, Primary Diamond Deposits of the World (Nedra, Moscow, 1998) [in Russian].
T. N. Kheraskova, D. V. Yakovlev, N. N. Pimanova, and O. S. Berezner, “Conjugation with the Central Asian Foldbelt: Interpretation of the 3DV and Tynda–Amurzet Transects,” Geotectonics 52 (1), 1–21, 2018.
F. A. Cook, D. J. White, A. G. Jones, D. W. S. Eaton, J. Hall, and R. M. Clowes, “How the crust meets the mantle: Lithoprobe perspectives on the Mohorovicic discontinuity and crust-mantle transition,” Can. J. Earth Sci. 47, 315–351 (2010).
B. L. N. Kennett, E. Saygin, T. Fomin, and R. Blewett, “Deep crustal seismic reflection profiling: Australia 1978–2011,” in ANUE Press and Commonwealth of Australia (Geoscience Australia), (Publ. House, Canberra, Australia. 2013).
M. Kuusisto, I. T. Kukkonen, P. Heikhinnen, and L. J. Pesonen, “Lithological interpretation of crustal composition in the Fennoscandian Shield,” Precambrian Res. 420, 283–299 (2006).
A. Singh and C. Singh, “Seismic imaging of the deep crustal structure beneath Eastern Ghats Mobile Belt (India): Crustal growth in the context of assembly of Rodinia and Gondwana supercontinents,” Precambrian Res. 331 (1), 105343 (2019).
A. P. Smelov and V. F. Timofeev, “The age of the North Asian cratonic basement: An Overview,” Gondwana Res., No. 12, 279–288 (2007).
G. Srijayanthi, M. Ravi Kumar, and V. K. Gahalaut, “A review of seismological research in India during the past five years (2015–2019),” Proc. Indian Natn. Sci. Acad. 86 (1), 531–552 (2020). https://doi.org/10.16943/ptinsa/2020/49794
C. A. Zelt and R. Smith, “Seismic traveltime inversion for 2D crustal velocity structure,” Geophys. J. Int. 108 (1), 16–34 (1992).
ACKNOWLEDGMENTS
The authors acknowledge S.V. Dunaev, L.I. Zhukova, A.N. Sidorenko, and K.Yu. Osipovich, geophysicists at Yakutskgeologiya production geological association (Yakutsk, Republic of Sakha (Yakutia)), for collaboration in 1988–1993 on the results of gravity surveys of the Aldan anteclise (scale 1 : 200 000).
The authors are grateful to A.N. Koltin, managing director of JSC Yakutskgeologiya (Yakutsk, Republic of Sakha (Yakutia)) for support of research activities.
The authors thank the anonymous reviewers for useful comments and the editor for thorough editing.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
The authors declare that they have no conflicts of interest.
Additional information
Translated by N. Astafiev
Rights and permissions
About this article
Cite this article
Stogny, G.A., Stogny, V.V. Structure of the Earth’s Crust in the Northeast Aldan Anteclise (Siberian Platform): Diamond Potential. Geotecton. 56, 280–293 (2022). https://doi.org/10.1134/S0016852122030086
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S0016852122030086