Zobrazeno 1 - 10 of 202 pro vyhledávání: '"E. A. Pavlov"'
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Akademický článek
Mechanochemical synthesis of intermetallic compounds in the system gallium – ruthenium
Autor: T. F. Grigoreva, E. A. Pavlov, P. A. Vitiaz, N. Z. Lyakhov
Publikováno v: Chimica Techno Acta, Vol 8, Iss 1 (2021)
The interaction of a solid inert metal Ru with liquid active metal Ga during mechanical activation in a high-energy planetary ball mill was studied using the X-ray diffraction and the high resolution scanning electron microscopy with energy dispersiv
Externí odkaz: https://doaj.org/article/9a5a7e76f1524c7abd17f1dc5fd6982a
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3
Seismic and density signs of mesozoic folding in the earth’s crust of the eastern passive margin of the Siberian craton (profile 3DV)
Autor: V. D. Suvorov, E. V. Pavlov, E. A. Melnik
Publikováno v: Russian Journal of Geophysical Technologies. :110-117
The results of a complex interpretation of seismic and gravity data along a part (500 km long) of the 3DV profile located in the transition zone from the Siberian Platform to the Verkhoyano-Kolyma fold system are considered. It crosses the Priverkhoy
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6f92d7971657e5fd8209dc0a869ffa04
https://doi.org/10.18303/2619-1563-2022-1-110
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6
The crust structure of the Aldano-Stanovoy shield according to the wide-angle seismic data (southern part of profile 3-DV)
Autor: V. D. Suvorov, E. A. Melnik, E. V. Pavlov
Publikováno v: Interexpo GEO-Siberia. 2:121-128
Significant differences in the layered-block structure of the earth's crust and the upper mantle, expressed in the distribution of localized seismic inhomogeneities of the Aldan and Stanovoi blocks and the zone of their junction, are revealed. A late
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::1d32e7ec8722a25ee52750ea4ee998cf
https://doi.org/10.33764/2618-981x-2022-2-2-121-128
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9
SEISMIC INHOMOGENEITIES IN THE UPPER CRUST OF THE ALDAN-STANOVOY SHIELD AND IN ITS TOTAL CRUST (PROFILE 3-DV)
Autor: V. D. Suvorov, E. A. Melnik, E. V. Pavlov
Publikováno v: Geodynamics & Tectonophysics. 14
In accordance with the detailed first-arrival data, the near-surface part of the Earth’s crust consists of three layers. The upper discontinuous layer is represented by the Mesocenozoic deposits in local basins. The two inhomogenous layers decrease
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5a79a0996b7178c3c9a183d77c235b0e
https://doi.org/10.5800/gt-2023-14-1-0682
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