Zobrazeno 1 - 10
of 14
pro vyhledávání: '"S. B. Nikolaeva"'
Autor:
S. B. Nikolaeva
Publikováno v:
Геодинамика и тектонофизика, Vol 13, Iss 5 (2022)
This paper presents the results of a study on traces of ancient earthquakes in the lake bottom sediments of eastern Fennoscandia (Kola region and Karelia). Based on the sediment cores from six lake basins located within large active structures of the
Externí odkaz:
https://doaj.org/article/9da33046394b4705afdcdbe9dffe2212
Publikováno v:
Геодинамика и тектонофизика, Vol 9, Iss 4, Pp 1189-1203 (2018)
The article describes the experience of using the GPR method to study the bottom sediments of Lake Upoloksha located in the Kola Peninsula, Russia. Such sediments are viewed as good archives of various Holocene geodynamic processes, including tectoni
Externí odkaz:
https://doaj.org/article/adb6c2cf09324e24982bd6a9b4802d79
Autor:
S. B. Nikolaeva
Publikováno v:
Doklady Earth Sciences. 506:S108-S115
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cdcfafd8727934067b1b3b7c8412c33
https://doi.org/10.1134/s1028334x22600293
https://doi.org/10.1134/s1028334x22600293
Publikováno v:
Russian Geology and Geophysics. 59:697-708
We present results of detailed paleoseismological research at the key site on the flank of the Lake Imandra depression (Kola region, northeast of the Fennoscandian Shield). Study of various groups of paleoseismic deformations in the fault zone and ap
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c96b0a98876cf6c10ec4b27ed177ab37
https://doi.org/10.1016/j.rgg.2018.05.008
https://doi.org/10.1016/j.rgg.2018.05.008
Publikováno v:
Doklady Earth Sciences. 473:308-312
Horizons with seismogenic sediments are revealed in the bottom sediments of the lake basins in the southwestern Kola Peninsula. In the borehole cores, they are represented by material that sharply differs from the overlying and underlying sediments:
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::68920801621e30003dc3a46a516d1c69
https://doi.org/10.1134/s1028334x17030072
https://doi.org/10.1134/s1028334x17030072
Publikováno v:
Doklady Earth Sciences. 471:1221-1225
Analysis of materials on the geological structure and tectonics of the White Sea depression area suggests that this depression existed in the Middle Pleistocene and was connected with the World Ocean. It is still impossible to determine the exact tim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a00e4d41bc61382eb07958e91d7fc484
https://doi.org/10.1134/s1028334x16120023
https://doi.org/10.1134/s1028334x16120023
Publikováno v:
Doklady Earth Sciences. 469:656-660
This paper considers the results of detailed paleoseismic and geological investigations in a key site in the wall of the Imandra Lake depression (Kola Peninsula Region, Northeast of the Fennoscandian Shield). Study of different groups of paleoseismic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8da2f20c25ccb298a0afa2b84d8b2b4
https://doi.org/10.1134/s1028334x16070138
https://doi.org/10.1134/s1028334x16070138
Autor:
S. B. Nikolaeva
Publikováno v:
Vestnik MGTU, Vol 19, Iss 1/1, Pp 110-122 (2016)
Results of studying secondary seismogenic deformations of the vibrational type (termed "seismites") in loose sediments of the north-eastern Baltic Shield (the Kola region) have been provided. The features, types, formation patterns and age of seismit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f3af8eeaa46a0d583d203698a9203384
http://vestnik.mstu.edu.ru/v19_1_1n64/14_Nikolaeva_110_122.pdf
http://vestnik.mstu.edu.ru/v19_1_1n64/14_Nikolaeva_110_122.pdf
Autor:
V. Ya. Yevzerov, S. B. Nikolaeva
Publikováno v:
Doklady Earth Sciences. 441:1598-1601
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::64f06d25ede0287532a63c19a43d9e3b
https://doi.org/10.1134/s1028334x11110249
https://doi.org/10.1134/s1028334x11110249
Autor:
S. B. Nikolaeva, V. Ya. Yevzerov
Publikováno v:
Doklady Earth Sciences. 421:792-795
The purpose of this work is to reconstruct terminal stages of the evolution of sheet and mountain glaciations in the Khibiny mountainous massif. We investigated a vast area of nepheline syenites of the Khibiny pluton in the southern Khibiny Massif. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a540de139966c00c41fec512f83eeaa8
https://doi.org/10.1134/s1028334x08050176
https://doi.org/10.1134/s1028334x08050176