Structural and chemical heterogeneity of colloform cassiterite and In, Pb, As minerals at the tin ores for the Verkhnee deposit (Primorye, Russia)
https://doi.org/10.32454/0016-7762-2019-4-11-18
Abstract
The colloform tin ores from the deposit Verkhnee at the Primorye have been studied with the aid of X- ray spectroscopic microanalysis and the scanning electron microscopy with the energy dispersive analyzer LINK-ISIS that allowed revealing the primary and the secondary zoning of a colloform cassiterite and to determine the phase composition of these formations. The primary zoning of the mineral forms at the early stage of the deposition of stannates from colloidal solutions and is characterized by the alternation of hydrostannates of various composition. The secondary zoning is superimposed zonality, and it forms at the process of the stannate crystallization. The metacolloidal varieties of concentric-zonal aggregates are produced by hydrostannates of Ca, Fe, Cu, In, of variable compositions, soluble in acids, in which the admixtures of As, Al, Si, Cd, Co, Sb, Zn, Ag are marked. Sn content according to the energy dispersive analysis is 42—54%. Infrared adsorption spectroscopy allowed finding out in hydrostannates the presence of the hydroxyl water at the area of the valence vibrations Sn-OH. In the colloform cassiterite a new phase Pb5 As2 O8 with various correlation of Pb and As in size 30—50 mk has been found.
About the Authors
N. V. GorelikovaRussian Federation
35, Staromonetny lane, Moscow 119017
V. I. Taskaev
Russian Federation
35, Staromonetny lane, Moscow 119017
V. A. Rassulov
Russian Federation
31, Staromonetny lane, Moscow 119017
References
1. Genkin A.D., Murav’eva I.V. Indite and dzalindite are new minerals of In. Zapiski RMO [Proceedings of the Russian Mineralogical Society], 1963, Part XCII, vol. 4, pp. 445-457. (In Russian)
2. Komarova G.N., Novorosova L.E. About the behavior of Sn and In in the colloform cassiterite aggregates at the Dzalinda deposit at the Little Khingnan Mountains. Geochemistry, 1959, no 8, pp. 716-720 (In Russian).
3. Marshukova N.K., Pavlovsky A.B., Sidorenko G.A. New mineral forms of tin ores, Mineralogy of ore deposits. Moscow, Nauka Publ., 1983, pp. 34-37 (In Russian)
4. Methodological recommendations N 40. Practice complex MSFUL-312 for the diagnostics of minerals. Moscow, VIMS Publ., 1993, 53 p. (In Russian).
5. Radkevich E.A. The metamorphism of Sinancha ores. Izvestia AN SSSR, Series geolog., 1948, pp. 131-140.
6. Chukhrov F.V. Colloides at the Earth’s crust. M., AN SSSR Publ., 1955, 671 p. (In Russian).
7. Shumskaya N.N. The identification of ore minerals on spectral reflection curves. L., Nedra Publ., 1985, 231 p. (In Russian).
8. Ahlfeld, F. and Reyes, J.M. Mineralogie von Bolivien. Gebruder Borntraeger, Berlin, 1938, 90 p.
9. Dunn P.J., Peacor D.R., and Sturman D. Paulmooreite, a new lead arsenite mineral from Langban, Sweeden. American Mineral, 1979, vol. 64, pp. 352-454.
10. Knopf, A.. Tungsten deposits of northwestern Inyo county, California, U.S. Geol. Survey Bull., 1916, 640, pp. 229-249.
11. Fries C. Tin Deposits of the Black Range, Catron and Sierra Counties, New Mexico. US Geol. Surv. Bull., 1940. no. 922-M. Pp. 355-370.
12. Roy R., Shafer M.W. Phases present and phase equilibrium in the system In2O3-*H2O. J. Phys. Chem., 1954, v. 58, p. 372.
Review
For citations:
Gorelikova N.V., Taskaev V.I., Rassulov V.A. Structural and chemical heterogeneity of colloform cassiterite and In, Pb, As minerals at the tin ores for the Verkhnee deposit (Primorye, Russia). Proceedings of higher educational establishments. Geology and Exploration. 2019;(4):11-18. (In Russ.) https://doi.org/10.32454/0016-7762-2019-4-11-18