Avdoninite, K2Cu5Cl8(OH)4 · H2O, a new mineral species from volcanic exhalations and the technogenic zone at volcanic-hosted massive sulfide deposits

Н. В. Чуканов1, Mikhail N. Murashko2, A. E. Zadov3, A. F. Bushmakin4
1Institute of Problems of Chemical Physics, Russian Academy of Sciences, Chernogolovka, Moscow oblast, Russia
2ZAO Systematic Mineralogy, St. Petersburg, Russia
3NPO Regenerator, Moscow, Russia
4Institute of Mineralogy, Ural Division, Russian Academy of Sciences, Miass, Chelyabinsk oblast, Russia

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A. F. Bushmakin and L. F. Bazhenova, “Avdoninite K2Cu5Cl8(OH)4: A New Mineral from Technogenic Zones at the Ural Massive Sulfide Ore Deposits,” Ural. Mineral. Sb, No. 8, 32–39 (1998).

I. A. Menyailov, L. P. Nikitina, and V. N. Shapar, Geochemistry of Exhalations from the Great Fissure Tolbachik Eruption (Nauka, Moscow, 1980) [in Russian].

S. I. Naboko and S. F. Glavatskikh, Posteruption Metasomatism and Ore Formation (Nauka, Moscow, 1983) [in Russian].

L. P. Vergasova and S. K. Filatov, “Exhalative Mineralization of the Great Fissure Tolbachik Eruption (GFTE, Kamchatka, 1975–1976),” in Posteruption Mineralization in Active Volcanoes of Kamchatka, Part 1, pp. 53–64 (1992) [in Russian].

L. P. Vergasova and S. K. Filatov, “Minerals of Volcanic Exhalation as a Specific Genetic Group,” Zap. Vseross. Mineral. O-va 122(4), 68–76 (1993).