Zobrazeno 1 - 7
of 7
pro vyhledávání: '"N. V. Lubnina"'
Autor:
N. V. Lubnina, O. V. Krylov, A. Yu. Bychkov, I. N. Modin, A. D. Skobelev, E. V. Kozlova, V. L. Kosorukov, M. V. Kosnyreva, N. I. Kosevich, A. Yu. Palenov
Publikováno v:
Georesursy, Vol 26, Iss 1, Pp 20-37 (2024)
As a result of generalization of geophysical studies, petro-paleomagnetic and structural-geomorphological analyses, as well as thermodynamic modeling, some features of ore formation in the hydrothermal system of Cape Fiolent (southwestern Crimea) und
Externí odkaz:
https://doaj.org/article/abb4326b2107431186ae8e1c711caebb
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 3, Pp 569-572 (2017)
Comparative analysis of the crustal evolution of the Early Precambrian Belomorian and Trans-North China orogens (Fig. 1) has shown [Slabunov et al., 2015] that: Both belts were formed by the superposition of two Precambrian orogenies. The earth crust
Externí odkaz:
https://doaj.org/article/5087fe5a37bc4117baf6b510fcbebb44
Autor:
O. V. Krylov, N. V. Lubnina, M. L. Vladov, I. N. Modin, G. V. Bryantseva, N. I. Kosevich, A. Yu. Palenov, A. D. Skobelev, A. I. Gushchin, V. O. Osadchiy, V. P. Evstigneev, A. A. Fadeev
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :152-166
A complex of geological and geophysical work was carried out to study fracturing in the Jurassic-Neogene rocks of the Heraclea Plateau, which included a field study of the Georgievsky fault zone, structural and geomorphological analysis; the geophysi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8ecdc1e11e9c79f622477897432bc61c
https://doi.org/10.33623/0579-9406-2022-6-152-166
https://doi.org/10.33623/0579-9406-2022-6-152-166
Publikováno v:
Moscow University Bulletin. Series 4. Geology. 1:3-10
Presents the results of magnetotelluric soundings acquired in 2020 along the profile Rzhev– Velikie Luki, in the suture zone of three parts of Precambrian crust of East European platform: Fennoscandia, Sarmatia and Volga–Ural. In the central part
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca79d06a458a954ad41a6c6df03ba046
https://doi.org/10.33623/0579-9406-2021-2-3-10
https://doi.org/10.33623/0579-9406-2021-2-3-10
Autor:
N. V. Lubnina, N. A. Tarasov
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :18-28
As a result of paleomagnetic studies Sariolian 2,4–2,3 Ga conglomerates of the Onega basin of the Karelian protoctaton, two characteristic components of magnetization have been separated. Mean direction of the medium-temperature component has a hea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10d84f87a201576c72a40bde56111e67
https://doi.org/10.33623/0579-9406-2018-6-18-28
https://doi.org/10.33623/0579-9406-2018-6-18-28
Autor:
V. S. Zakharov, N. V. Lubnina
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :3-13
The secondary (metachronous) component of magnetization isolated in the Precambrian complexes of the Karelian craton have been analyzed. The mean directions of high temperature components (deviations from the true direction) depending on the contribu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::306a6c81bebd9f48c94cec392cfcb1bb
https://doi.org/10.33623/0579-9406-2018-5-3-13
https://doi.org/10.33623/0579-9406-2018-5-3-13
Autor:
N. V. Lubnina, A. I. Slabunov
Publikováno v:
Moscow University Bulletin. Series 4. Geology. :3-15
New paleomagnetic and isotopic-geochronological data obtained for Neoarchean Onega granulite complex, were used to reconstruct the position of the Karelian craton in the Neoarchean supercontinent Kenorland. Geological correlations were made for the K
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4d5f418532fc1dde2df64f2477d8329
https://doi.org/10.33623/0579-9406-2017-5-3-15
https://doi.org/10.33623/0579-9406-2017-5-3-15