Temperature conditions of ore formation at the Deputatskoye deposit
Abstract
Tin ores of the Deputatskoye deposit (northeastern Yakut ASSR) were formed during five stages: quartz-tourmaline, cassiterite-silicate-quartz, quartz-sulfide, quartz-carbonate-sulfide, and carbonate. Cassiterite was deposited from solutions of all stages, but its main mass was formed in the second stage in close association with vein quartz, tourmaline, fluorite, chlorite, and wolframite. Cassiterites of the second (main productive) stage were the subject of our study.
Область исследования:
(Archived) Without section
Funding:
None
References
- Belousov V. V., Gzovsky M. V. Experimental Tectonics. Nedra, 1964 (in Russian)
- Lir Yu. V. Some features of manifestation of primary zonality of mineralization at Deputatskoye deposit. In the collection: Ore Formation and Its Connection with Magmatism. Sb. Rudoobrazovanie i ego svyaz' s magmatizmom Yakutsk, Book Publishing House Yakutsk. knizhn. izd-vo, 1969 (in Russian)
- Nekrasov I. Ya. Main features of mineralization of Deputatskoye tin deposit. Tr. In-ta geologii Yakutsk, f-la SO AN SSSR Proc. Institute of Geology, Yakutsk Branch of the Siberian Branch of the AS USSR, issue 7, 1960 (in Russian)
- Ryabov V. K. Temperature conditions of crystallization of cassiterite in tin ore deposits of the Far East according to the thermosonic method. Geologiya rudn. m-nii Geology of Ore Deposits, 1966, No. 3 (in Russian)
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