The latest neotectonic structures in the Eastern Dagestan

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Late orogenic structural plan was distinguished with orotectonic method in addition to two well-known structural plans, i.e., late geosyncline and early orogenic, in the territory of Eastern Dagestan, which is the western near-orogenic flank of the Tersk-Dagestan foredeep. This structural plan unites the youngest neotectonic structures and determines the main features of the modern relief. It is characterized by the predominance of blocky structures associated both with the activation of arched orogenic uplift and with the taphrogenic influence of developing Caspian depression. The block structures of this structural plan determine localization of modern exogenous processes including geohazards and disruptures, which must be taken into account upon construction, irrigation and other economic activities. Therefore, the study of this structural plan is not only of theoretical, but also of practical significance.

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作者简介

S. Nesmeyanov

Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences

Email: voa49@mail.ru
俄罗斯联邦, Ulanskii per. 13, bld. 2, Moscow, 101000

O. Voeykova

Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences

编辑信件的主要联系方式.
Email: voa49@mail.ru
俄罗斯联邦, Ulanskii per. 13, bld. 2, Moscow, 101000

参考

  1. Bolysov, S.I. [Tectonic deformation of the Early Khvalyn Sea coastline at the Dagestan coast of the Caspian Sea]. Vestnik MGU, ser. 5. Geografiya, 1980, no. 2, pp. 80—82. (in Russian)
  2. Brod, I.O., Polster, L.A., Nesmeyanov, D.V. [Geostructural zoning and prospects of oil and gas potential of the CisCaucasus]. In: [Geological structure and prospects for the oil and gas content in the CisCaucasus]. Annex to the journal Geologiya nefti i gaza, 1958, no. 8, pp. 11—63. (in Russian)
  3. [Geology of the USSR]. Vol. 9, North Caucasus. Moscow-Leningrad, Gosgeolizdat, 1947, part 1, 600 p. (in Russian)
  4. [Geology of the USSR]. Vol. 9, North Caucasus. Moscow, Nedra Publ., 1968, part 1, 759 p. (in Russian)
  5. [A map of the latest tectonics in the South of the USSR]. Scale 1 : 1 000 000. L.P. Polkanova, ed., Leningrad, Kartfabrika VAGT, 1972. (in Russian)
  6. Korzhenkov, A.M., Gadzhiev, M.S., Ovsyuchenko, A.N. et al. [Traces of seismic activity on architectural monuments in Derbent, Dagestan]. Geofizicheskie protsessy i biosfera, 2020, vol. 19, no. 1, pp. 5—29. (in Russian)
  7. Krivolutskii, A.E. [Phenomena of Upper Pliocene levelling in Mountainous Dagestan]. Vestnik MGU, ser. 5. Geografiya, 1960, no. 3, pp. 22—29. (in Russian)
  8. Leontiev, O.K., Maev, E.G., Rychagov, G.I. [Geomorphology of the shores and the bottom of the Caspian Sea]. Moscow, MSU Publ., 1977, 210 p. (in Russian)
  9. Milanovskii, E.E. [The newest tectonics of the Caucasus]. Moscow, Nedra Publ., 1968, 484 p. (in Russian)
  10. Mirzoev, D.A., Sharafutdinov, F.G. [Geology of oil and gas deposits in Dagestan]. Makhachkala, Dagestan Publ., 1986, 312 p. (in Russian)
  11. Nesmeyanov, S.A. [Correlation of continental strata]. Moscow, Nedra Publ., 1977, 198 p. (in Russian)
  12. Nesmeyanov, S.A. [Neostructural zoning of the North-Western Caucasus]. Moscow, Nedra Publ., 1992, 254 p. (in Russian)
  13. Nesmeyanov, S.A. [Orotectonic method]. Moscow, Mittel Press Publ., 2017, 376 p. (in Russian)
  14. Nesmeyanov, S.A., Voeikova O.A. [New data on the types of the youngest newest structures in Eastern Dagestan]. Doklady AN, 1994, vol. 338, no. 3, pp. 365—367. (in Russian)
  15. Nesmeyanov, S.A., Nikitin, M.Yu., Voeikova, O.A., Komarevskaya, M.N. [Neostructural zoning of the Russian part of the Eastern segment of the Greater Caucasus megavault (advanced research for engineering survey)]. Geoeckologiya, 2024, no 2, pp. 3—18.
  16. [Oil and gas formation and accumulation in the Eastern Caucasus]. Moscow, Nauka Publ., 1990, 206 p. (in Russian)
  17. Nikiforov, L.G. [Structural geology of sea coasts]. Moscow, MSU Publ., 1977, 175 p. (in Russian)
  18. Rengarten, V.P. [Geological observations in the Kaitago-Tabasaran and Darginsky regions of Dagestan]. In: [Transactions in general and applied geology]. Moscow, 1927, issue 66, 56 p. (in Russian)
  19. Rychagov, G.I. [Pleistocene history of the Caspian Sea]. Extended abstract of Doctoral Sci. (Geogr.) Diss., 1977, 62 p. (in Russian)
  20. Svitoch, A.A. [Fluctuations of the Caspian Sea level in the Pleistocene (classification and systematic description)]. In: [The Caspian Sea: paleogeography and geomorphology of the Caspian region in the Pleistocene]. Moscow, Nauka Publ., 1991, pp. 5—99. (in Russian)
  21. Svitoch, A.A., Yanina, T.A. [Quaternary deposits of the Caspian Sea coasts]. Moscow, 1996, 268 p. (in Russian)
  22. Sobornov, K.O. [Sub-thrust fault zones of oil and gas accumulation as a new object of oil and gas exploration in Foothill Dagestan]. Geologiya nefti i gaza, 1988, no 2, pp. 8—12. (in Russian)
  23. [Tectonics of Dagestan (explanatory note to the Tectonic map of Dagestan, scale 1 : 500 000)]. Leonov Yu.G., Ed.]. In: [Transactions of the Institute of Geology, Dagestan Research Centre, RAS]. issue 60. Makhachkala, ALEF Publ., 2012, 130 p. (in Russian)
  24. Fedorov, P.V. [Stratigraphy of Quaternary sediments and the history of the Caspian Sea development]. Moscow, AN SSSR Publ., 1957, 308 p. (in Russian)
  25. Fedorov, P.V. [Pleistocene of the Ponto-Caspian Sea]. Moscow, Nauka Publ., 1978, 165 p. (in Russian)
  26. Chepalyga, A.L., Amirkhanov, Kh.A., Sadchikova, T.A. et al. [Geochronology of the Olduvai sites of Mountainous Dagestan in the sediments of the Akushinskaya formation of the Eopleistocene]. Bull. KICHP, 2012, no. 72, pp. 73—94. (in Russian)
  27. Sharkov, V.V. [Geology of the underwater slope of the western coast of the Caspian Sea (from Makhachkala to the Kura River mouth)]. Moscow-Leningrad, Nauka Publ., 1964, 430 p. (in Russian)
  28. Yanina, T.A. [Neopleistocene of the Ponto-Caspian: biostratigraphy, paleogeography, correlation]. Moscow, Moscow, MSU Publ., 2012, 26 p. (in Russian)
  29. Yanina, T.A., Svitoch, A.A. [Malacofauna of reference sections of the Pleistocene in Dagestan]. In: [The Caspian Sea: issues of geology and geomorphology]. Moscow, Nauka Publ., 1990, pp. 41—52. (in Russian)

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2. Fig. 1. Fragment of the map of the latest tectonics of the South of the USSR (edited by L.P. Polkanova [5]). 1 - isolines of the total amplitudes of neotectonic movements, drawn along the base of the latest deposits, 2 - the boundary of the distribution of the latest deposits, 3 - the latest ruptures; 4-7 — local uplifts: 4 — expressed in relief, 5-7 — containing deposits: 5 — oil, 6 — oil and gas, 7 — gas condensate (numbers — structure numbers: 233 — Shevchenkovskoye, 234 — Volohovskoye, 235 — Brigadirovskoye, 236 — South Brigadirovskoye, 237 — Sabinskoye, 238 — North Golubovskoye, 239 — Druzhelyubovskoye, 240 — Zaitsevskoye, 241 — Olgovskoye, 242 — West Nezhinskoye, 244 — Khimoryabushinskoye, 245 — Tvanskoye, 246 — Doroginskoye, 247 — Krapivnyanskoye, 248 — Khomovskoye, 249 — South Doroginskoye, 251 — Parafiyevskoye.

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3. Fig. 2. Geological and geomorphological profiles of Eastern Dagestan. The profile lines are shown (I, II, III) in Fig. 3. Legend: 1-2 - boundaries: 1 - Makhachkala orogenic wing and mega-arch of the Greater Caucasus, 2 - Sergokala and Derbent regional structural stages; 3 - faults, indicating the direction of displacement along them and the amplitude of displacement of erosion-denudation levels; 4 - cirque-shaped faults; 5-8 - the newest deposits: 5 - Akchagyl stage, 6 - Apsheron stage, 7 - Middle-Upper Quaternary complex, 8 - Upper Quaternary; 9-10 - indices of structures: 9 - faults, 10 - block; 11-12 — erosion-denudation levels: 11 — Akchagyl, 12 — Apsheron.

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4. Fig. 3. The youngest neotectonic structures of Eastern Dagestan: A — block, B — faults and flexures. Legend: 1-2 — boundaries: 1 — Makhachkala orogenic wing and mega-arch of the Greater Caucasus, 2 — Sergokala and Derbent regional structural steps and the Sulak Depression; 3 — mega-arch of the Greater Caucasus; 4-8 — structures of the high Sergokala regional structural step: 4 — horsts, 5 — horst steps, 6 — structural steps, 7 — graben steps, 8 — grabens, 9-13 — structures of the Derbent low regional structural step: 9 — uplifts, 10 — structural steps, 11 — high cirque-shaped steps, 12 — cirque-shaped steps, 13 — low cirque-shaped steps; 14 — Sulak Depression; 15 — indices of the newest block structures (see Table 2); 16–18 — faults and flexures: 16 — normal faults, 17 — cirque faults, 18 — flexures; 19 — indices of the newest fault structures and flexures (see Table 3); 20 — lines of structural-geomorphological profiles (see Fig. 2).

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5. Fig. 4. Structural and geomorphological scheme of the Makhachkala-Caspian area. Legend: 1 — boundaries of the Sergokala and Derbent regional structural steps and the Sulak Depression; 2-5 — structures of the high Sergokala regional structural step: 2 — horsts, 3 — horst-steps, 4 — structural steps, 5 — grabens; 6-9 — structures of the Derbent low regional structural step: 6-7 — within the Makhachkala uplift: 6 — horst, 7 — structural step; 8 — step; 9 — lowered step; 10-12 — structures of the Sulak Depression; 10 — high step, 11 — step, 12 — lowered step; 13 — indices of the newest block structures (see Table 2); 14-16 — faults and flexures: 14 — normal faults, 15 — cirque faults, 16 — flexures; 17 — indices of the newest fault structures and flexures (see Table 3); 18 — Holocene local plicative structures and their indices (see Table 4). The Sergokalinsky regional stage is separated here from the Derbent regional stage by the South Makhachkala (2) and West Achisuysky (4) normal faults.

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6. Fig. 5. Structural and geomorphological scheme of the Derbent area. Legend: 1 — boundary of the Sergokala and Derbent regional structural stages; 2-5 — structures of the high Sergokala regional structural stage: 2 — horsts, 3 — horst-stages, 4 — structural stages, 5 — grabens; 6-10 — structures of the Derbent low regional structural stage: 6-8 — within the Derbent uplift: 6 — high stage, 7 — stage; 8 — low stage; 9 — high cirque-shaped stages, 10 — cirque-shaped stages; 11 — indices of the newest block structures (see Table 2); 12-14 — faults and flexures: 12 — normal faults, 13 — cirque-shaped faults, 14 — flexures; 15 — indices of the newest fault structures and flexures (see Table 3) 16 — Holocene local plicative structures and their indices (see Table 4).

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