Zobrazeno 1 - 10
of 41
pro vyhledávání: '"V V Shcherbakova"'
Autor:
V. V. Shcherbakova, R. V. Veselovskiy, G. V. Zhidkov, N. A. Aphinogenova, A. V. Samsonov, A. V. Stepanova, M. A. Smirnov
Publikováno v:
Učënye Zapiski Kazanskogo Universiteta. Seriâ Estestvennye Nauki, Vol 165, Iss 4, Pp 537-549 (2023)
Giant mafic dykes are the key markers of the Earth’s evolution in the Precambrian and have been the subject of extensive research. This article presents the results of the paleomagnetic, rock-magnetic, and paleointensity Banc studies of the Great D
Externí odkaz:
https://doaj.org/article/b4eac3da8a40409c97f4f21dc3341a3d
Autor:
V. V. Shcherbakova, V. Yu. Vodovozov, G. V. Zhidkov, N. A. Aphinogenova, N. V. Sal’naya, G. L. Leichenkov
Publikováno v:
Izvestiya, Physics of the Solid Earth. 58:859-881
Autor:
D. V. Metelkin, E. V. Vinogradov, V. V. Shcherbakova, V. A. Vernikovsky, S. M. Zakharov, K. E. Nagovitsin
Publikováno v:
Doklady Earth Sciences. 506:710-715
Autor:
D Thallner, V V Shcherbakova, V G Bakhmutov, V P Shcherbakov, G V Zhidkov, I B Poliachenko, A J Biggin
Publikováno v:
Geophysical Journal International. 231:474-492
SUMMARY Changes in the geomagnetic field over geologic timescales can be used to study the evolution and processes of its sources in Earth's deep interior. As a stark contrast to the geomagnetic field behaviour of the recent past, the field in the la
Publikováno v:
Geophysical Journal International. 230:1132-1146
SUMMARY Changes in palaeosecular variation, dipole moment and polarity reversal frequency are salient features of the Earth’s magnetic field over the geological past, yet how these changes are linked by the geodynamo remains controversial. To furth
Autor:
V. V. Shcherbakova, G. V. Zhidkov, V. P. Shcherbakov, I. V. Golovanova, K. N. Danukalov, R. Yu. Salmanova
Publikováno v:
Izvestiya, Physics of the Solid Earth. 57:900-912
Autor:
E. M. Bobrovnikova, F. Lhuillier, V. P. Shcherbakov, V. V. Shcherbakova, G. V. Zhidkov, I. E. Lebedev, B. Eid, V. E. Pavlov
Publikováno v:
Journal of Geophysical Research: Solid Earth. 127
Autor:
Andrew J. Biggin, Valera P. Shcherbakov, V. V. Shcherbakova, Daniele Thallner, Vladimir Bakhmutov, G. V. Zhidkov
Publikováno v:
GEOPHYSICAL JOURNAL INTERNATIONAL
SUMMARY The time-averaged geomagnetic field is generally purported to be uniformitarian across Earth history—close to a geocentric axial dipole, with average strength within one order of magnitude of that at present. Nevertheless, recent studies ha
The Precambrian period occupies ≈ 85% of the Earth’s geological history and accommodates all the main formation stages of the Earth as a planet, including the emergence of its magnetic field. Variations in the time-averaged geomagnetic dipole mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::932eb6f092bd542020ded4f1420fa93e
https://doi.org/10.5194/egusphere-egu2020-5776
https://doi.org/10.5194/egusphere-egu2020-5776
Autor:
A. M. Pasenko, A. V. Shatsillo, Vladimir Pavlov, Sergey V. Malyshev, V. V. Shcherbakova, V. I. Powerman
Publikováno v:
Izvestiya, Physics of the Solid Earth. 54:782-805
Representative paleomagnetic collections of Lower Cambrian rocks from the northern and eastern regions of the Siberian platform are studied. New evidence demonstrating the anomalous character of the paleomagnetic record in these rocks is obtained. Th