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Geology
B. N. Abramov
Journal Article
Petrochemistry of the Paleoproterozoic Udokan copper-bearing sedimentary complex
Lithology and Mineral Resources, 2008, Volume 43, Number 1, Pages 37-43
Sources and provenances of lower proterozoic terrigenous rocks of the Udokan group, Southern Kodar-Udokan depression: Results of Sm-Nd isotopic investigations
V. N. Podkovyrov, A. B. Kotov, A. M. Larin, L. N. Kotova and V. P. Kovach, et al.
Doklady Earth Sciences, 2006, Volume 408, Number 1, Pages 518-522
Formation Conditions and ore potential of black shales of the Udokan Group, East Siberia
Lithology and Mineral Resources, 2011, Volume 46, Number 4, Pages 353-362
Periodicity of copper accumulation in the Earth’s sedimentary shell
I. F. Gablina and Yu. M. Malinovskii
Lithology and Mineral Resources, 2008, Volume 43, Number 2, Pages 136-153
A new type of gold-platinum-copper mineralization in northern Transbaikalia
B. I. Gongalsky, Yu. G. Safonov, N. A. Krivolutskaya, V. Yu. Prokof’ev and A. A. Yushin
Doklady Earth Sciences, 2007, Volume 415, Number 1, Pages 671-674
Forms of concentration of ore elements in carbon-rich metasomatites
Yu. V. Danilova, T. G. Shumilova and B. S. Danilov
Doklady Earth Sciences, 2006, Volume 411, Number 1, Pages 1263-1266
Intensity and extensiveness of ore mineralization in structures of tectonostratigraphic terranes
A. A. Sidorov and A. V. Volkov
Doklady Earth Sciences, 2008, Volume 420, Number 1, Pages 592-596
Aspects of genetic formational typification of metalliferous highly carbonaceous sedimentary complexes
V. I. Starostin and O. V. Yapaskurt
Moscow University Geology Bulletin, 2007, Volume 62, Number 3, Pages 131-142
Modeling of geochemical processes occurred during the formation of the Schlema deposit, Erzgebirge. II. Formation of pre-uranium veins
Vikt. L. Barsukov
Geochemistry International, 2006, Volume 44, Number 12, Pages 1191-1214
Transport species and accumulation of chemical elements in hydrothermal fluids
B. N. Ryzhenko
Geology of Ore Deposits, 2008, Volume 50, Number 3, Pages 155-191
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