NEOTECTONICS OF THE MANYCH TROUGH

A. A. Svitoch; R. R. Makshaev

doi:10.15356/0435-4281-2013-1-43-52

NEOTECTONICS OF THE MANYCH TROUGH

A. A. Svitoch, R. R. Makshaev

https://doi.org/10.15356/0435-4281-2013-1-43-52

Full Text:

PDF (Rus) |

Generate QR code

Abstract

In the Pleistocene Manych Trough experienced sustained lowering overall amplitude of up to 40-50 m at a speed of 0.1 mm/year, the most active in its central part. Among the local structures of the most dynamic deflection was Manych Gudulovskaya depression and elevation Zunda-Tolga. In time, the largest neotectonic activity occurs at the end of early, middle of the middle and late Pleistocene. In Holocene and modern times the amplitude of neotectonic movements, possibly due to the short duration of these periods.

Keywords

Manych, though, trench, tectonics, putting down

About the Authors

A. A. Svitoch

Lomonosov Moscow State University
Russian Federation
Geographical Department

R. R. Makshaev

Lomonosov Moscow State University
Russian Federation
Geographical Department

References

1. Belousov T.P., Anman S.V. Morphostructural plan and tectonic movements of the Stavropolskaiy upland in the quaternary and today. Geomorphologiya (Geomorphology RAS), 1999, no. 4, pp. 56-69 (in Russ.).

2. Geologiya SSSR (Geology of the USSR). Moscow: Nedra (Publ.), 1970, Vol. XLVI. 666 p.

3. Panina L.V. Newest structures of the Scythian Plate. Vesn. Mosc. Univ. Ser.6: Geol., 2009, no. 1, pp. 23-31 (in Russ.).

4. Popov G.I. Pleystotsen chernomorsko-kaspiyskih prolivov (Pleistocene of the Black Sea – Caspian Sea gates). Moscow: Nauka (Publ.), 1983, 213 p.

5. Svitoch A.A., Yanina T.A., Novikova N.G., Khomenko A.A. Pleystotsen Manycha (Pleistocene of the Manych (questions of the structure and evolution). Moscow: Rosselhozakademia (Publ.), 2010, 133 p.

6. Sudarikov U.A. Zakonomernosti razmeshcheniya nefti I gaza epigertsinskih platform yuga SSSR (Oil and gas location in epi-Hercynian platform of the south part of the USSR). Moscow: Nedra (Publ.), 1964, Vol. 2, 475 p.

7. Svitoch A.A., Selivanov A.O., Yanina T.A. Paleogeograficheskie sobytiya pleystocena Ponto-Kaspiya I Sredizemnomor’ya (Paleogeographical events of the Pleistocene Ponto-Caspian and Mediterranean). Moscow: Rosselhosakademia (Publ.), 1989, 289 p.

8. Svitoch A.A., Menabde I.V., Yanina T.A. Paleohydrology of the Manych in the late

9. Pleistocene. Vodn. Resur., 1991, no. 1, pp. 77–91 (in Russ.).

10. Leonov N.V., Chepalyga A.A. Salskiy border of the Caspian Khvalyn basin, in Aktualnye problem paleogeografii I stratigrafii pleystotsena (Actual problems of the paleogeography and stratigraphy of the Pleistocene). Moscow: Rosselhosakademia (Publ.), 2010, pp. 45-46.

11. Danilevskiy N.Ya. Extraction from letter about journey on Manych. Zap.RGO, 1869, Vol. 2, pp. 139-180 (in Russ.).

12. Bogachev V.V. Steppes of the Manych basin. Geologia, 1903, V. 22, Iss. 2, pp. 73-162 (in Russ.)

13. Goretskiy G.I. Towards the paleogeography of Priazov and Western Primanych in the usunlaro-hyrkanckiy and burtasskiy ages. Vopr. Geogr., 1953, no. 33, pp. 190–221 (in Russ.).

14. Lisitsin K.I. Geological guide to Manych, in Putevoditel’ ekskursii 2-oy assoc. po izuch. Chetver. Perioda Evropy (Guide to excursions of the Second intern. ass. on the Europian Quant. Period). Moscow-Leningrad: Gos. nauch-tekh. izd-vo (Publ.), 1939, pp. 204-225.

Review

For citations:

Svitoch A.A., Makshaev R.R. NEOTECTONICS OF THE MANYCH TROUGH. Geomorfologiya. 2013;(1):43-52. (In Russ.) https://doi.org/10.15356/0435-4281-2013-1-43-52