Zobrazeno 1 - 10
of 16
pro vyhledávání: '"D. S. Zykov"'
Publikováno v:
Геодинамика и тектонофизика, Vol 14, Iss 4 (2023)
Consideration is being given to the Onega Paleoproterozoic structure (Onega synclinorium, OS) as a tectonotype of intraplate negative structures, which experience intermittent subsidence over a long period of time. The paper presents a model of the O
Externí odkaz:
https://doaj.org/article/8d608820dc584ee0a7aaa72fc56f3398
Autor:
D. S. Zykov, A. V. Poleshchuk, E. A. Kotova, A. O. Agibalov, E. A. Manuilova, A. A. Khmarenko
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :28-34
According to drilling data, the internal structure of the Mozyr salt cryptodiapir has been reconstructed, the main elements of which are strongly compressed folds with radially arranged layers on the wings, complicating domes and inter-dome depressio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2b8a0bc7e1237980b74a8cced548e1c
https://doi.org/10.33623/0579-9406-2022-5-28-34
https://doi.org/10.33623/0579-9406-2022-5-28-34
Autor:
D. S. Zykov, A. V. Poleshchuk, E. A. Kotova, A. O. Aghibalov, E. A. Manuilova, A. A. Khmarenko
Publikováno v:
Moscow University Geology Bulletin. 77:641-647
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49082dda8cdeecbddad74f201bc3bcd9
https://doi.org/10.3103/s0145875222060175
https://doi.org/10.3103/s0145875222060175
Autor:
S. Yu. Kolodyazhny, M. M. Pevzner, A. V. Poleshchuk, D. S. Zykov, M. G. Leonov, I. M. Varentsov, P. V. Ivanov
Publikováno v:
Journal of Volcanology and Seismology. 15:399-413
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9833475a2beab22e822a64c047dd3b06
https://doi.org/10.1134/s0742046321060063
https://doi.org/10.1134/s0742046321060063
Publikováno v:
Geotectonics. 55:473-501
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea84033887f22806b4951979d04fd400
https://doi.org/10.1134/s0016852121040099
https://doi.org/10.1134/s0016852121040099
Publikováno v:
Geotectonics. 54:1-18
The general tectonic features of the Baltic-Mezen zone developed along the border of the Fennoscandian shield and the Russian Plate in the north of the East European platform, are considered. The geophysical remote methods and structural analysis wer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cf8f59aa29086e138208f3e56dc8ba1f
https://doi.org/10.1134/s0016852120010057
https://doi.org/10.1134/s0016852120010057
Publikováno v:
Геотектоника. :62-86
Tectonics, morphological features and development stages of Belomorian-Severodvinsk shear zone (north-western part) found in the East European platform are considered. We traced the shear zone (length ≈1000 km) from NW to SE from the Baltic shield
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c35fa8a2345e387f5bbc5f2eb2af7ffc
https://doi.org/10.31857/s0016-853x2019162-86
https://doi.org/10.31857/s0016-853x2019162-86
Publikováno v:
Geotectonics. 53:60-83
The tectonics, morphological features, and development stages of the Belomorian‒Severodvinsk shear zone (northwestern part) found in the East European Platform are considered. We traced the shear zone (length ≈ 1000 km) from NW to SE from the Bal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5854c615836907c9466756733aae9805
https://doi.org/10.1134/s0016852119010047
https://doi.org/10.1134/s0016852119010047
Autor:
V. G. Spungin, D. S. Zykov
Publikováno v:
Journal of Volcanology and Seismology. 12:56-66
This paper summarizes the observations of microseismic emissions by these authors in several areas of the Russian part of the Fennoscandian Shield to assess the potential of microseismicity to determine the present-day activity of local features in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f0882f45225d8987814551f107bdea4
https://doi.org/10.1134/s0742046318010062
https://doi.org/10.1134/s0742046318010062
Publikováno v:
Geomorphology RAS. :79-89
Karpinski and Trollford–Kanin lineaments are located at the junction of the East European and the Western Arctic platforms. Spatial patterns of depressions and elevations in this region exhibit the deformations of morphostructures by opposite in di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b04fbffd47e22892c3f68034f761ffe
https://doi.org/10.15356/0435-4281-2017-2-79-89
https://doi.org/10.15356/0435-4281-2017-2-79-89