[1]
G.N. Vitvitskiy: The Far East. Physical-geographical characteristics. Ch. Climate. USSR Acad. Sci., Moscow (1961), 93-115.
Google Scholar
[2]
I.K. Karpov: The physicochemical computer modeling in geochemistry. Nauka, Novosibirsk (1981), p.247.
Google Scholar
[3]
R. Khorn: Marine chemistry. Mir, Moscow (1972), p.398.
Google Scholar
[4]
V.P. Zvereva: Ecological effects of the hypergene processes at tin deposits of the Far East. Dalnauka, Vladivostok (2008), p.166.
Google Scholar
[5]
P.V. Elpatyevskiy, V.A. Chudaeva, E.F. Zazykina, V.S. Arzhanova: Role of the technogenic factor in the ionic flow formation: (on example of one of the rivers of Primorsky Krai). Geochemistry of hypergene zone and technical human activity. FESC, USSR Acad. Sci., Vladivostok (1976). pp.17-27.
Google Scholar
[6]
N.I. Grekhnev, V.I. Ostapchuk, L.F. Kislitsin: Heavy metals in the geosystems of mining area and tin-polymetallic ore processing in the south Far East. The effect of the mining industry processes on the environmental objects. Dalnauka, Vladivostok (1998). pp.12-31.
Google Scholar
[7]
V.A. Chudaeva: Migration of chemical elements in the Far East waters. Dalnauka, Vladivostok (2002), p.391.
Google Scholar
[8]
D.S. Potapov, S.S. Potapov: Technogenesis and mineralogy of technogenesis: Definitions and examples of research facilities. Mineralogy of technogenesis. IMin RAS 2004, Miass (2004), pp.209-219.
Google Scholar
[9]
V.P. Zvereva: Ecological effects of the technogenesis at tin deposits of the Far East. Ore deposits of the continental margins. Dalnauka, Vladivostok (2000). pp.263-274.
Google Scholar