Zobrazeno 1 - 10
of 28
pro vyhledávání: '"O. A. Avchenko"'
Publikováno v:
Russian Geology and Geophysics. 61:689-699
—Unique magnesian–aluminous ultrabasic sapphirine–spinel and garnet gedritites of the Aulandzha block were studied. The deepest part of the Archean Stage of the Omolon massif is exposed in this district. The gedritites differ strongly in petroc
Publikováno v:
Геология рудных месторождений. 61:64-84
Composition and genesis of arsenium-antimony sulfosalts of lead from the gold-bearing ores of the Berezitovoe deposit located in the eastern part of Mongol-Okhotsk orogenic belt (Upper Amur Area) were considered. Lead sulfosalts (Cu and Pb) are prese
Publikováno v:
Geology of Ore Deposits. 61:256-273
Composition and genesis of arsenium-antimony sulfosalts of lead from the gold-bearing ores of the Berezitovoe deposit located in the eastern part of Mongol-Okhotsk orogenic belt (Upper Amur Area) were considered. Lead sulfosalts (Cu and Pb) are prese
Publikováno v:
Russian Journal of Pacific Geology. 12:174-189
Spinel–sapphirine reaction structures are studied in detail in the sapphirine gedritites which form a small segregation in one of the garnet metaultramafic bodies framing the Aulandzha charnockitic dome (the pre-Riphean basement of the Omolon Massi
Publikováno v:
Vestnik of Institute of Geology of Komi Science Center of Ural Branch RAS. 3:14-19
Publikováno v:
Doklady Earth Sciences. 467:402-407
New data on the composition of jordanite–geocronite Pb–Sb–As sulfosalts in the vein–disseminated gold ore at the Berezitovoe deposit were provided. Within the studied quartz–sulfide sample, some grains of Pb–Sb–As sulfosalts, uniform in
Publikováno v:
Russian Geology and Geophysics. 56:1133-1147
The problem of modeling of real parageneses has been solved by minimization of Gibbs thermodynamic potential for metapelites of the Okhotsk granulite complex. Model mineral assemblages completely reproduce the composition of minerals and their modal
Publikováno v:
Geology of Ore Deposits. 56:15-34
The geological position, composition of mineral assemblages, and typomorphism of major minerals from garnet-bearing rocks at the Berezitovoe gold-base-metal deposit in the Upper Amur Region have been studied in detail. These are ore-bearing metasomat
Autor:
O. V. Avchenko, A. S. Vakh, I. A. Aleksandrov, I. N. Kapitonov, T. A. Velivetskaya, Nikolay A. Goryachev
Publikováno v:
Doklady Earth Sciences. 453:1117-1120
1117 The results of the study of stable oxygen, sulfur, and lead isotopes in rocks and ores of the Berezitovoe gold–polymetallic deposit in the Upper Amur allow� ing us to clarify the debatable problems of its genesis are discussed in this paper.
Autor:
O. V. Avchenko, V. I. Kiselev, Yanchen Yang, N. A. Goryachev, A. S. Vakh, V. G. Khomich, Song-Qing Ye, V. I. Gvozdev, Guobin Zhang
Publikováno v:
Doklady Earth Sciences. 450:575-582
New data on the isotopic age of zircons from metamorphic and igneous rocks are given for the Berezitovoe and Kirovskoe deposits located in the eastern margin of the Selenga-Stanovoi orogenic belt. The zircons were studied with the LA-ICP-MS method in