Silica and alumina transfer in supercritical aqueous fluids and growing of topaz monocrystals in them

Author:

Balitsky V. S.,Balitsky D. V.,Balitsky S. D.,Aurisicchio C.,Roma M. A.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference13 articles.

1. V. B. Naumov, V. I. Kovalenko, G. F. Ivanova, and N. V. Vladykin, “The Genesis of Topaz: Evidence from Microinclusions,” Geokhimiya, No. 3, 323–331 (1977).

2. Yu. B. Shapovalov, “Mineral Equilibria in the System K2O-Al2O3-SiO2-H2O-HF at T=300–600°C and P=1000 bar,” in Contributions to Physicochemical Petrology, Issue XV: Hydrothermal Processes and Mineral Equilibria (Nauka, Moscow, 1988), pp. 160–167 [in Russian].

3. G. P. Zaraiskii, Yu. B. Shapovalov, Yu. B. Soboleva, et al., “Physicochemical Environment of Greisenization at the Akchatau Deposit: Evidence from Geological and Experimental Data,” in Experimental Problems in Geology (Nauka, Moscow, 1994), pp. 371–419 [in Russian].

4. I. M. Naumko and V. A. Kalyuzhnyi, “Typomorphism of Topaz from a Zone of Leaching and Recrystallization in the Volhynia Cavity-Type Pegmatites,” Mineral. Zh. 3(3), 52–61 (1981).

5. A. Michel-Levy and J. Wyart, “Reproduction Ertificielle Sous Pression Elevee de la Cassiterite, de la Topaze, du Corindon, de la Cryolie et de la Chiolite,” C. R. Acad. Sci. Paris 224, 166–168 (1947).

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