Zobrazeno 1 - 10
of 38
pro vyhledávání: '"K. Yu. Murashov"'
Publikováno v:
Литосфера, Vol 20, Iss 2, Pp 254-270 (2020)
Research subject. The Mississippi Valley type deposits make up about a third of the global balance of lead and zinc reserves, resources and production. Additionally, silver, antimony, arsenic, barium, bismuth, cadmium, cobalt, gallium, indium, mercur
Externí odkaz:
https://doaj.org/article/b864c9f5be5f4d91bb76725565ffbfba
Publikováno v:
Doklady Earth Sciences. 510:276-280
Autor:
A. V. Volkov, N. E. Savva, V. Yu. Prokofiev, B. I. Ishkov, K. Yu. Murashov, A. A. Dolomanova-Topol, N. V. Sidorova
Publikováno v:
Geology of Ore Deposits. 65:107-132
Autor:
N. S. Bortnikov, A. V. Volkov, A. L. Galyamov, I. V. Vykentiev, A. V. Lalomov, K. Yu. Murashov
Publikováno v:
Geology of Ore Deposits. 64:313-328
Publikováno v:
Journal of Volcanology and Seismology. 16:323-333
Publikováno v:
Doklady Earth Sciences. 506:625-629
Autor:
A. A. Sidorov, N. G. Lyubimtseva, N. E. Savva, K. Yu. Murashov, V. Yu. Prokofiev, A. V. Volkov, N. V. Sidorova
Publikováno v:
Geology of Ore Deposits. 63:185-211
The Gol’tsovoe Ag–Pb–Zn-deposit (1600 t silver in ores with an average grade of 1025 g/t Ag) is located on the southeastern flank of the Dukat mining district, at the junction of the Balygychan–Sugoi rift trough and the Okhotsk–Chukotka Vol
Publikováno v:
LITHOSPHERE (Russia). 21:222-238
Research subject. The gold-sulphide-quartz deposits of Central Chile are typical prospecting objects, having small ore intervals (from the first tens of centimetres to 1 m), intermittent and nested ore distribution and extremely uneven gold contents.
Autor:
N. S. Bortnikov, A. V. Volkov, A. L. Galyamov, I. V. Vikentyev, A. V. Lalomov, K. Yu. Murashov
Publikováno v:
Geology of Ore Deposits. 65:190-190
Publikováno v:
Geology of Ore Deposits. 63:34-53
The Burgali deposit is located in the Paleozoic Kedon volcanic belt (KVB) within the Omolon cratonic terrane. The orebodies of the Burgali deposit are veined and stockwork-type. The studies of the wallrock metasomatites demonstrate that the erosional