Zobrazeno 1 - 9
of 9
pro vyhledávání: '"E. N. Perova"'
Publikováno v:
Geology of Ore Deposits. 64:78-103
Autor:
A. I. Brusnitsyn, E. N. Perova, O. S. Vereshchagin, S. N. Britvin, N. V. Platonova, V. V. Shilovskhikh
Publikováno v:
Geology of Ore Deposits. 63:772-792
Autor:
E. F. Letnikova, A. I. Brusnitsyn, S. I. Shkolnik, Alexander V. Ivanov, E. N. Perova, E. N. Lepekhina
Publikováno v:
Doklady Earth Sciences. 497:195-199
Isotope study of ore-bearing rocks at Fe–Mn rift deposits of the Atasu and Zhezdy (Dzhezdy) ore districts in Central Kazakhstan has been carried out for the first time. The Atasu felsic effusive rocks (Ushkatyn-1 deposit), synchronous to ore genesi
Publikováno v:
Geology of Ore Deposits. 61:663-670
The results of experimental modeling of the arsenic transition from natural arsenides to mobile oxidized species in the near-surface environment are discussed. The experiment has been carried out with the samples collected from the dump of the Schlem
Publikováno v:
Zapiski RMO (Proceedings of the Russian Mineralogical Society). 147:28-39
Autor:
E. N. Perova, Anatoly N. Zaitsev
Publikováno v:
Geology of Ore Deposits. 59:584-591
Carbonatites from the Oldoinyo Lengai volcano, northern Tanzania, are unstable under normal atmospheric conditions. Owing to carbonatite interaction with water, the major minerals—gregoryite Na2(CO3), nyerereite Na2Ca(CO3)2, and sylvite KCl—are d
Publikováno v:
Eurasian Soil Science. 50:961-970
The mineralogy of soils and parent rocks of the Iremel Ridge has been studied by the methods of micromorphology, laser diffraction, computed X-ray microtomography, and X-ray fluorescence analysis. In hard rock and soil, the major minerals have been i
Publikováno v:
Doklady Earth Sciences. 415:954-960
The First Find of Buried Low-Temperature Hydrothermal Deposits in the Mid-Atlantic Ridge Rift Valley
Autor:
M. P. Davydov, E. N. Perova, P. A. Aleksandrov, Yu. S. Polekhovskii, Fedor Maksimov, T. A. Semkova, V. Yu. Kuznetsov
Publikováno v:
ResearcherID
Buried ferromanganese deposits (FMD) were recovered in the course of vibrodrilling at Station 1361 within the terrace on the western slope of the Mid-Atlantic Ridge (MAR) rift valley at 13 ° N during Cruise 24 of the R/V Professor Logachev in 2004.
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