Zobrazeno 1 - 10
of 66
pro vyhledávání: '"G. A. Ovchinnikova"'
Autor:
G. V. Ovchinnikova, A. S. Ovchinnikova
Publikováno v:
Вестник Московского государственного лингвистического университета. Гуманитарные науки. :182-191
Publikováno v:
Crystallography Reports. 65:757-761
Dependencies of the complex permittivity of chromium-doped ferroelectric triglycine sulfate crystals (TGS + Cr) have been measured using dielectric spectroscopy method in a frequency range of 1–107 Hz and a temperature range of 23–60°C upon heat
Autor:
A. S. Ovchinnikova, G. V. Ovchinnikova
Publikováno v:
Philology at MGIMO. 21:100-109
For the first time the article presents a comparative analysis of intercultural communication on the example of the analysis of stereotypes of the French, Italian and Russian languages. Students who study Russian as a foreign language, use it for int
Publikováno v:
Stratigraphy and Geological Correlation. 27:538-554
The Pb–Pb isotope age and the Sr isotope signature of the Upper Riphean sedimentary limestones from the south of the Yenisei Range on the western margin of the Siberian Craton were obtained. The Pb–Pb age of carbonate deposits of the Dadykta Form
Autor:
A. L. Tolstikhina, A. P. Eremeev, V. V. Grebenev, N. V. Belugina, E. S. Ivanova, G. I. Ovchinnikova
Publikováno v:
Crystallography Reports. 64:774-779
The temperature evolution of the dielectric spectra of TGS–TGS + Cr crystals (TGS stands for triglycine sulfate) with a periodic distribution of chromium impurity (Cr3+) has been studied in comparison with nominally pure TGS crystals in the frequen
Autor:
T. L. Turchenko, V. P. Kovach, Igor M. Gorokhov, T. S. Zaitseva, I. M. Vasil’eva, G. V. Ovchinnikova, G. V. Konstantinova, M. M. Arakelyants, A. B. Kuznetsov
Publikováno v:
Стратиграфия. 27:3-30
The 2–5, 0.6–2, 0.3–0.6, 0.2–0.3 and 0.1–0.2 µm clay subfractions (SFs) separated from two shale samples of the Upper Riphean Inzer Formation, the southern Urals, were studied by the TEM, XRD, and U–Pb, Sm–Nd, Rb–Sr and K–Ar isotop
Autor:
A. B. Kuznetsov, G. V. Konstantinova, M. M. Arakelyants, I. M. Vasil’eva, T. S. Zaitseva, V. P. Kovach, Igor M. Gorokhov, G. V. Ovchinnikova, T. L. Turchenko
Publikováno v:
Stratigraphy and Geological Correlation. 27:133-158
Clay subfractions (SFs) with particles size of 2–5, 0.6–2.0, 0.3–0.6, 0.2–0.3, and 0.1–0.2 μm of two shale samples (Upper Riphean Inzer Formation, South Urals) are studied using transmission electron microscopy, X-ray diffractometry (XRD),
Autor:
Kuo-Lung Wang, I. M. Vasil’eva, N. A. Sergeeva, G. V. Ovchinnikova, S. D. Velikoslavinskii, V. P. Kovach, A. B. Kotov, A. A. Sorokin, A. M. Larin, S.-L. Chun, N. N. Mel’nikov, E. B. Sal’nikova, V. M. Savatenkov
Publikováno v:
Petrology. 26:447-468
The geochemistry, geochronology, and isotope geochemical systematics (Nd, Sr, Hf, and Pb) of the granitoids of the Pozdnestanovoy complex of the Dzhugdzhur–Stanovoy superterrane of the Central Asia fold belt were investigated. It was shown that the
Publikováno v:
Doklady Earth Sciences. 481:1040-1044
For the first time, the age of magnesite in the Lower Riphean Bakal Formation of the Southern Urals is determined by the U—Pb (Pb—Pb) method: it is equal to 1366 ± 47 Ma (MSWD = 18). The stage of magnesite formation of the Bakal ore field was as
Publikováno v:
Precambrian Research. 298:157-173
Neoproterozoic sedimentary records reveal a poorly documented, ∼150 m.y. time interval, between ∼1000 and 850 Ma, that limit our understanding of C and Sr isotope variations in seawater and thus operation of the biogeochemical carbon cycle, chang